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  • 2020-2024  (9,586)
  • 1985-1989  (11)
  • 2024  (9,586)
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  • 1
    Publication Date: 2024-06-27
    Description: Invasive alien species (IAS) threaten biodiversity and human well-being. These threats may increase in the future, necessitating accurate projections of potential locations and the extent of invasions. The main aim of the IAS prototype Digital Twin (IAS pDT) is to dynamically project the level of plant invasion at habitat level across Europe under current and future climates using joint species distribution models. The pDT detects updates in data sources and versions of the datasets and model outputs, implementing the FAIR principles. The pDT’s outputs will be available via an interactive dashboard. All input and output data will be freely accessible.
    Keywords: Invasive alien species ; Digital Twin ; climate change ; joint species distribution models ; Dynamic Data-Driven Application Systems ; workflows
    Repository Name: National Museum of Natural History, Netherlands
    Type: info:eu-repo/semantics/article
    Format: application/pdf
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  • 2
    Publication Date: 2024-06-27
    Description: The prevalence in allergic diseases has increased considerably in the past decades. An important trigger of the symptoms of allergic rhinitis (hay fever) is the pollen of wind-pollinating plants. This pollen is developed by plants and is released into the air where it gets exposed to environmental influences and air pollution. We investigated the chemical changes to pollen that occur after release from the flower in a rural (Veluwe) and an urban (Amsterdam) site in the Netherlands using Fourier Transform Infrared (FTIR) spectroscopy. During the spring/summer of 2020 (during the COVID pandemic) the pollen of nine taxa (Alnus, Betula, Fagus, Fraxinus, Pinus, Plantago, Poaceae, Quercus and Salix) were collected directly from flowers and the air (using a mobile sampler). FTIR spectra were obtained for multiple individual pollen grains for each taxa. The spectra obtained from airborne pollen collected at the rural vs. urban sites did not show any statistical difference. This is possibly a result of a reduced difference in pollutant concentrations between the two sites due to the COVID-19-lockdown measures were in place. However, consistent differences in the FTIR spectra recovered from airborne vs. flower pollen were recorded for all pollen taxa. After the release from the flower the chemical composition of the pollen changed: (i) polysaccharides are converted to monosaccharides; (ii) protein concentration and/or nitration/oxidation level is altered; (iii) lipids are modified and/or reduced in concentration. These changes may alter the allergenicity of the pollen and suggest that further work on the allergenic nature of airborne pollen is required.
    Keywords: Pollen ; Airborne ; FTIR spectroscopy ; Air pollution
    Repository Name: National Museum of Natural History, Netherlands
    Type: info:eu-repo/semantics/article
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  • 3
    Publication Date: 2024-06-27
    Description: Documenting the seasonal temperature cycle constitutes an essential step toward mitigating risks associated with extreme weather events in a future warmer world. The mid-Piacenzian Warm Period (mPWP), 3.3 to 3.0 million years ago, featured global temperatures approximately 3°C above preindustrial levels. It represents an ideal period for directed paleoclimate reconstructions equivalent to model projections for 2100 under moderate Shared Socioeconomic Pathway SSP2- 4.5. Here, seasonal clumped isotope analyses of fossil mollusk shells from the North Sea are presented to test Pliocene Model Intercomparison Project 2 outcomes. Joint data and model evidence reveals enhanced summer warming (+4.3° ± 1.0°C) compared to winter (+2.5° ± 1.5°C) during the mPWP, equivalent to SSP2-4.5 outcomes for future climate. We show that Arctic amplification of global warming weakens mid- latitude summer circulation while intensifying seasonal contrast in temperature and precipitation, leading to an increased risk of summer heat waves and other extreme weather events in Europe’s future.
    Keywords: Aragonitic bivalve shells ; Sea-surface temperature ; North-Sea ; Atmospheric circulation ; PLIOMIP2 simulations ; Arctic amplification ; Marine heatwaves ; Summer drought ; Wadden Sea ; Pliocene
    Repository Name: National Museum of Natural History, Netherlands
    Type: info:eu-repo/semantics/article
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  • 4
    Publication Date: 2024-06-27
    Description: Background: Predicting and explaining species occurrence using environmental characteristics is essential for nature conservation and management. Species distribution models consider species occurrence as the dependent variable and environmental conditions as the independent variables. Suitable conditions are estimated based on a sample of species observations, where one assumes that the underlying environmental conditions are known. This is not always the case, as environmental variables at broad spatial scales are regularly extrapolated from point-referenced data. However, treating the predicted environmental conditions as accurate surveys of independent variables at a specific point does not take into account their uncertainty. Methods: We present a joint hierarchical Bayesian model where models for the environmental variables, rather than a set of predicted values, are input to the species distribution model. All models are fitted together based only on point-referenced observations, which results in a correct propagation of uncertainty. We use 50 plant species representative of the Dutch flora in natural areas with 8 soil condition predictors taken during field visits in the Netherlands as a case study. We compare the proposed model to the standard approach by studying the difference in associations, predicted maps, and cross-validated accuracy. Findings: We find that there are differences between the two approaches in the estimated association between soil conditions and species occurrence (correlation 0.64-0.84), but the predicted maps are quite similar (correlation 0.82-1.00). The differences are more pronounced in the rarer species. The cross-validated accuracy is substantially better for 5 species out of the 50, and the species can also help to predict the soil characteristics. The estimated associations tend to have a smaller magnitude with more certainty. Conclusion: These findings suggests that the standard model is often sufficient for prediction, but effort should be taken to develop models which take the uncertainty in the independent variables into account for interpretation.
    Repository Name: National Museum of Natural History, Netherlands
    Type: info:eu-repo/semantics/article
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  • 5
    Publication Date: 2024-06-27
    Description: Long-term food security and agricultural sustainability depend on protecting the eco-evolutionary processes that select for local adaptation in crops. Since seed systems structure how people acquire seed, institutional and social changes influence evolutionary processes within agroecosystems. Since World War II, the rise of professional breeding has bifurcated seed systems into traditional and formal systems, which has negatively affected agrobiodiversity, crop evolution, and agricultural sustainability. In traditional seed systems, farmers often save seed from plants that best provide desired qualities, selecting landrace crop varieties to adapt to local environmental conditions. In formal or centralized seed systems, farmers buy seeds bred primarily for maximizing yield under ideal conditions. When farmers source seeds externally,evolutionary processes underlying local adaptation are disrupted. Here, we argue that traditional seed systems provide important evosystem services, or the evolutionary processes resulting from the maintenance and use of genetic diversity that benefit society. We present a framework on how seed systems influence the evolutionary processes that enable local adaptation, which is necessary for sustainable agriculture. We discuss how changes in human values underlying traditional and formal seed systems can alter evolutionary processes that underlie local adaptation. We conclude that developing policies that support people in managing ecological and evolutionary processes within seed systems is needed to address current and future challenges of global food security and agricultural sustainability.
    Keywords: agriculture ; agroecology ; biodiversity ; ecosystem services ; evolution ; insects ; landrace ; seed systems
    Repository Name: National Museum of Natural History, Netherlands
    Type: info:eu-repo/semantics/article
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  • 6
    Publication Date: 2024-06-27
    Description: The contribution of deterministic versus stochastic processes to the spatio-temporal assembly of soil microbial communities in tropical forests requires quantification so that responses to climate change may be accurately projected. Here we report the spatio-temporal composition of soil fungal communities in a topographically homogeneous forest area in central Amazonia. Soil fungal communities have a greater turnover in space than over time. Stochastic processes are inferred to dominate in the rainy season and deterministic processes in the dry season. Our study highlights the importance of spatial heterogeneity in the absence of environmental gradients and its relationship with seasonal patterns that modulate spatial heterogeneity and contribute to environmental determinism versus stochasticity for fungal community assembly. This baseline may serve to assess deviations in community patterns caused by changes in biotic interactions with above-ground vegetation, such as those resulting from shifts in taxonomical/functional composition of trees driven by climate change.
    Repository Name: National Museum of Natural History, Netherlands
    Type: info:eu-repo/semantics/article
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  • 7
    Publication Date: 2024-06-27
    Description: Terrestrial orchids are a group of genetically understudied, yet culturally and economically important plants. The Orchidinae tribe contains many species that produce edible tubers that are used for the production of traditional delicacies collectively called ‘salep’. Overexploitation of wild orchids in the Eastern Mediterranean and Western Asia threatens to drive many of these species to extinction, but cost- effective tools for monitoring their trade are currently lacking. Here we present a custom bait kit for target enrichment and sequencing of 205 novel genetic mark- ers that are tailored to phylogenomic applications in Orchidinae s.l. A subset of 31 markers capture genes putatively involved in the production of glucomannan, a water-soluble polysaccharide that gives salep its distinctive properties. We tested the kit on 73 taxa native to the area, demonstrating universally high locus recovery irrespective of species identity, that exceeds the total sequence length obtained with alternative kits currently available. Phylogenetic inference with concatenation and coalescent approaches was robust and showed high levels of support for most clades, including some which were previously unresolved. Resolution for hybridiz- ing and recently radiated lineages remains difficult, but could be further improved by analysing multiple haplotypes and the non-exonic sequences captured by our kit, with the promise to shed new light on the evolution of enigmatic taxa with a complex speciation history. Offering a step-up from traditional barcoding and universal markers, the genome-wide custom loci targeted by Orchidinae-205 are a valuable new resource to study the evolution, systematics and trade of terrestrial orchids.
    Keywords: Orchidinae ; phylogenomics ; species identification ; target capture ; wildlife trade
    Repository Name: National Museum of Natural History, Netherlands
    Type: info:eu-repo/semantics/article
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  • 8
    Publication Date: 2024-06-27
    Description: Se presenta la cuarta parte de las claves ilustradas para la clasificación de los cangrejos bra- quiuros (Crustacea, Brachyura) de Cuba. Se incluyen las claves y figuras originales de las especies pertenecientes a la Section Eubrachyura, Subsection Heterosomata (final) para la clasificación de las familias Domeciidae (un género y una especie); Panopeidae (10 géneros y 18 especies); Linnaeoxanthidae (un género y una especie); Pseudorhombilidae (11 géne- ros y 16 especies) y Xanthidae (17 géneros y 19 especies), citadas para Cuba.
    Description: The fourth part of the illustrated keys for the classification of the brachyuran crabs (Crus- tacea, Brachyura) of Cuba is presented. The keys and original figures of the species belon- ging to the Section Eubrachyura, Subsection Heterosomata (final) for the classification of the families Domeciidae (1genus and 1 species); Panopeidae (10 genera and 18 species); Linnaeoxanthidae (un género y una especie); Pseudorhombilidae (11 genera and 16 spe- cies) and Xanthidae (17 genera and 19 species) cited for Cuba, are included.
    Description: Published
    Description: Refereed
    Keywords: Claves dicotómicas ilustradas ; Cangrejos braquiuros de Cuba ; Illustrated dichotomous keys ; Brachyuran crabs ; Cuba
    Repository Name: AquaDocs
    Type: Journal Contribution
    Format: 101-114 pp.
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  • 9
    Publication Date: 2024-06-27
    Description: The brachyuran crab Charybdis hellerii is originally from the Pacific; nevertheless, the spe- cies has been introduced to tropical waters globally. Its initial sighting in the Western Atlan- tic was documented in 1990 based on specimens collected in Cuba in 1987. In this paper, we present findings of C. hellerii from two localities in eastern Cuba: Santiago de Cuba and Taco bays. Up to this point, the species has solely been documented in estuaries in Cuba, and it likely exists throughout the entire archipelago. Given its feeding behaviour and extensive distribution, encompassing areas within the National Park Alejandro de Humboldt, this species can be key in the formulation of conservation plans for Cuban marine ecosystems.
    Description: El cangrejo braquiuro Charybdis hellerii es originario del Pacífico; sin embargo, la espe- cie ha sido introducida en aguas tropicales a nivel mundial. Su primera aparición en el Atlántico Occidental se registró en 1990 en base a especímenes recolectados en Cuba en 1987. En este artículo, presentamos los hallazgos de C. hellerii en dos localidades en Cuba oriental: las bahías de Santiago de Cuba y Taco. Hasta el momento, la especie solo ha sido registrada en estuarios en Cuba y es probable que esté presente en todo el archipiélago. Dada su conducta alimentaria y su amplia distribución, que incluye áreas dentro del Par- que Nacional Alejandro de Humboldt, esta especie puede ser clave en la formulación de planes de conservación para los ecosistemas marinos cubanos.
    Description: Published
    Description: Refereed
    Keywords: Bioinvasions ; Caribbean Sea ; Conservation ; Decapoda ; Portunidae ; Bioinvasiones ; Mar Caribe ; Conservación
    Repository Name: AquaDocs
    Type: Journal Contribution
    Format: 95-100pp.
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  • 10
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    PANGAEA
    In:  GEOMAR - Helmholtz Centre for Ocean Research Kiel
    Publication Date: 2024-06-27
    Description: Raw data acquired by position sensors on board RV METEOR during expedition M196 were processed to receive a validated master track which can be used as reference of further expedition data. During M196 the motion reference unit Kongsberg SeaTex AS MRU-5 combined with Kongsberg SeaTex AS Seapath 320 and two C and C Technologies GPS receivers C-NAV3050 were used as navigation sensors. Data were downloaded from DAVIS SHIP data base (https://dship.bsh.de) with a resolution of 1 sec. Processing and evaluation of the data is outlined in the data processing report. Processed data are provided as a master track with 1 sec resolution derived from the position sensors' data selected by priority and a generalized track with a reduced set of the most significant positions of the master track.
    Keywords: 1 sec resolution; CT; DAM_Underway; DAM Underway Research Data; GoCW; M196; M196-track; Meteor (1986); Underway cruise track measurements
    Type: Dataset
    Format: application/zip, 79.7 MBytes
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  • 11
    Publication Date: 2024-06-27
    Description: Passive acoustic monitoring (PAM) data were collected by recorder SV1019 of type Sono.Vault (manufactured by develogic GmbH, Hamburg, Germany) at 20.9757 ° S, 5.9845 ° E, mooring AWI247-3, in the eastern Atlantic Ocean off Namibia. During a deployment period from November 2012 to November 2014, passive acoustic data were collected from November 2012 to May 2013 (recording period) by SV1019 off Namibia. The recorder was moored at 736 m depth and scheduled to record continuously at a sample rate of 5,333 Hz. Further details about the data acquisition and processing of this data set can be found in the accompanying metadata file (see Additional metadata) as well as the data processing report (see Data Processing Report). Passive acoustic data archived here represent data processing Level 1+, according to the standards defined in the associated Standard Operation Procedure (SOP) Glossary (Thomisch et al. 2023a). Further information on data processing with regard to data preparation and standardization can be found in the associated SOP Part 1: Data preparation and standardization (Thomisch et al. 2023b).
    Keywords: ANT-XXIX/1; ANT-XXX/1.2; Audio file; Audio file (File Size); DATE/TIME; DEPTH, water; MOOR; Mooring; Passive acoustic recorder Sono.Vault, develogic GmbH; Polarstern; PS81; PS81/017-2; PS88/049-1; PS88.2; South Atlantic Ocean
    Type: Dataset
    Format: text/tab-separated-values, 190 data points
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  • 12
    Publication Date: 2024-06-27
    Description: Passive acoustic monitoring (PAM) data were collected by recorder SV1008 of type Sono.Vault (manufactured by develogic GmbH, Hamburg, Germany) at 20.9633 ° S, 5.9767 ° E, mooring AWI247-2, in the eastern Atlantic Ocean off Namibia. During a deployment period from November 2011 to November 2012, passive acoustic data were collected from November 2011 to August 2012 (recording period) by SV1008 off Namibia. The recorder was moored at 741 m depth and scheduled to record continuously at a sample rate of 5,333 Hz. Further details about the data acquisition and processing of this data set can be found in the accompanying metadata file (see Additional metadata) as well as the data processing report (see Data Processing Report). Passive acoustic data archived here represent data processing Level 2+ (see the associated data processing report), deviating from Standard Operation Procedure (SOP) Glossary (Thomisch et al. 2023a). Further information on data processing with regard to data preparation and standardization can be found in the associated SOP Part 1: Data preparation and standardization (Thomisch et al. 2023b).
    Keywords: ANT-XXIX/1; ANT-XXVIII/1; Audio file; Audio file (File Size); DATE/TIME; DEPTH, water; Mooring (long time); MOORY; Passive acoustic recorder Sono.Vault, develogic GmbH; Polarstern; PS79; PS79/029-1; PS81; PS81/017-1; South Atlantic Ocean
    Type: Dataset
    Format: text/tab-separated-values, 275 data points
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  • 13
    Publication Date: 2024-06-27
    Description: Passive acoustic monitoring (PAM) data were collected by recorder SV1005 of type Sono.Vault (manufactured by develogic GmbH, Hamburg, Germany) at 69.005° S, 6.9815° W, mooring AWI244-2, in the Weddell Sea, Atlantic sector of the Southern Ocean. During a deployment period from December 2010 to December 2012, passive acoustic data were collected from December 2010 to January 2011 (recording period) by SV1005 as part of the Hybrid Antarctic Float Observing System (HAFOS) in the Weddell Sea. The recorder was moored at 1003 m depth and scheduled to record continuously at a sample rate of 5,333 Hz. Further details about the data acquisition and processing of this data set can be found in the accompanying metadata file (see Additional metadata) as well as the data processing report (see Data Processing Report). Passive acoustic data archived here represent data processing Level 2+, deviating from the standards defined in the associated Standard Operation Procedure (SOP) Glossary (Thomisch et al. 2023a). Further information on data processing with regard to data preparation and standardization can be found in the associated SOP Part 1: Data preparation and standardization (Thomisch et al. 2023b).
    Keywords: ANT-XXIX/2; ANT-XXVII/2; Audio file; Audio file (File Size); AWI244-2; DATE/TIME; DEPTH, water; HAFOS; Hybrid Antarctic Float Observation System; MOOR; Mooring; Passive acoustic recorder Sono.Vault, develogic GmbH; Polarstern; PS77; PS77/068-2; PS81; PS81/067-1; Weddell Sea
    Type: Dataset
    Format: text/tab-separated-values, 23 data points
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  • 14
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    PANGAEA
    In:  Izaña Atmospheric Research Center, Meteorological State Agency of Spain
    Publication Date: 2024-06-27
    Keywords: Anemometer; BARO; Barometer; Baseline Surface Radiation Network; BSRN; Code; DATE/TIME; Dew/frost point; Geopotential of a standard isobaric surface; High cloud; HYGRO; Hygrometer; IZA; Izaña; Low/middle cloud amount; Low cloud; Middle cloud; Monitoring station; MONS; Past weather1; Past weather2; Present weather; Station pressure; Temperature, air; Tenerife, Spain; Thermometer; Total cloud amount; Visual observation; Wind direction; Wind speed
    Type: Dataset
    Format: text/tab-separated-values, 1018 data points
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  • 15
    Publication Date: 2024-06-27
    Description: Photomicrographs of representative mineralogy are here presented for each unit defined in our study. Unit A is dominated by quartz and feldspar whereas clay minerals, clinopyroxene and micas are in minor proportions (S4.1 and S4.2). Quartz, especially polycrystalline quartz, is dominant within the Unit B whereas micas and clinopyroxene are low in abundance (S4.3 and S4.4). Unit C is characterized by a high content in clay minerals as well as feldspar and monocrystalline quartz (S4.5). Unit D is characterized by a high content of polycrystalline quartz (chert) and feldspar (S4.6 and S4.7).
    Keywords: Binary Object; Binary Object (File Size); Binary Object (MD5 Hash); Binary Object (Media Type); deep-marine sediments; File content; petrography analysis; zircon age dating
    Type: Dataset
    Format: text/tab-separated-values, 28 data points
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  • 16
    Publication Date: 2024-06-27
    Description: U-Pb zircon age dating was applied on U-channel samples (30cc) that were collected from sandy deposits in cores from IODP Site C0024 (one sample; frontal Nankai accretionary Prism), ODP Site 1177 (two samples; Western Shikoku Basin) and IODP sites C0011 (three samples) and C0012 (one sample; Eastern Shikoku Basin). Detrital zircon U-Pb ages were measured using the London Thermochronology Research Group facilities at UCL based on a New Wave Nd: YAG 213 nm laser ablation system coupled plasma-mass spectrometry. Real time U-Pb were processed using GLITTER data reduction software. Repeated measurements of external zircon standard Plesovice (TIMS reference 337.13 +/-0.37 Myr ago) and NIST 612 silicate glass were used to correct for instrumental mass bias and depth-dependent inter-element fractionation of Pb, Th, and U. 206Pb/238U ages are used for those grain younger than 1 Ga, and for zircon grains older than 1,000 Ma we used the 207Pb/206Pb ages to determine the crystallization age. To better constrain the sediment provenance along the Nankai subduction zone, we integrated published U-Pb zircon age to our study. These include (1) potential sediment sources, e.g., Nagara, Yodo, Tenryu, Kiso and Fuji rivers from Clift et al. (2013) (https://doi.pangaea.de/10.1002/tect.20033), the Yangtze and Yellow rivers from Huang et al. (2020) (https://doi.pangaea.de/10.3390/min10050398), the Shimanto Complex from Shibata et al. (2008) (https://doi.org/10.1111/j.1440-1738.2008.00626.x) and the Sanbagawa Belt from Tsutsumi et al. (2009) (https://doi.org/10.2465/jmps.080416) and (2) published zircon ages from the frontal accretionary prism ((ODP sites 1176 and 1177 and IODP sites C0006E and C0007E; Clift et al., 2013) (https://doi.pangaea.de/10.1002/tect.20033).
    Keywords: 190-1177A; 322-C0011B; 322-C0012A; 358-C0024D; Age; Age, 206Pb/238U Lead-Uranium; Age, 207Pb/206Pb Lead-Lead; Age, 207Pb/235U Lead-Uranium; Age, dated; Age, dated standard error; Age, standard error; Chikyu; deep-marine sediments; DEPTH, sediment/rock; DRILL; Drilling/coring; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Exp322; Exp358; GLITTER - data reduction software; Grains; IODP Depth Scale Terminology; Joides Resolution; Latitude of event; Lead-206/Uranium-238, standard error; Lead-206/Uranium-238 ratio; Lead-207/Lead-206 ratio; Lead-207/Lead-206 ratio, standard error; Lead-207/Uranium-235, standard error; Lead-207/Uranium-235 ratio; Leg190; Longitude of event; NanTroSEIZE Plate Boundary Deep Riser 4; NanTroSEIZE Stage 2: Subduction Input; Percentage; petrography analysis; Philippine Sea; Sample code/label; Thorium; Thorium/Uranium ratio; Uranium; zircon age dating
    Type: Dataset
    Format: text/tab-separated-values, 13881 data points
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  • 17
    Publication Date: 2024-06-27
    Description: Ternary diagrams are commonly used in Earth Sciences to represent numerical data as ratios of three components. For our study, ternary provenance diagrams were created in Microsoft Excel directly from the raw point-count data of sand samples from IODP sites C0002N and C0002P (presented in doi:10.1594/PANGAEA.969334). Raw point-count data were recalculated as volumetric proportions by summing up quartzose, feldspar and lithic fragment framework constituents. Other grains identified in the point counting were excluded from these calculations but were retained for later use in stratigraphic correlation.
    Keywords: 348-C0002N; 348-C0002P; Calculated; Chikyu; deep-marine sediments; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DRILL; Drilling/drill rig; Event label; Exp348; Feldspar, volumetric proportion; Latitude of event; Lithic grains, sedimentary, volumetric proportion; Lithic grains, total, volumetric proportion; Lithic grains, unstable, total, volumetric proportion; Lithic grains, volcanic, volumetric proportion; Longitude of event; Nankai Trough; NanTroSEIZE Plate Boundary Drilling 3; petrography analysis; Quartz, monocrystalline, volumetric proportion; Quartz, polycrystalline, volumetric proportion; Quartz, total, volumetric proportion; Sample code/label; zircon age dating
    Type: Dataset
    Format: text/tab-separated-values, 880 data points
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  • 18
    Publication Date: 2024-06-27
    Description: The METEOR expedition M188 SONETT II, conducted in the southeast Atlantic, represents a collaborative initiative within the TRR181 framework. It brings together various observational projects with the goal of integrating diverse process studies to observe multiple energy compartments. This cruise coincided with the 'fast-sampling' (CalVal) phase of the Surface Water and Ocean Topography (SWOT) satellite mission. During the expedition, a total of 30 Hereon Surface Drifters were deployed.
    Keywords: Changing Earth – Sustaining our Future; DATE/TIME; DEPTH, water; DRIFT; Drifter; Eastern South Atlantic; Energy Transfers in Atmosphere and Ocean; Helmholtz_ChangingEarth; LATITUDE; LONGITUDE; M188; M188_3-1; Meteor (1986); Sample code/label; SFB181; SONETT II
    Type: Dataset
    Format: text/tab-separated-values, 29987 data points
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  • 19
    Publication Date: 2024-06-27
    Description: The METEOR expedition M188 SONETT II, conducted in the southeast Atlantic, represents a collaborative initiative within the TRR181 framework. It brings together various observational projects with the goal of integrating diverse process studies to observe multiple energy compartments. This cruise coincided with the 'fast-sampling' (CalVal) phase of the Surface Water and Ocean Topography (SWOT) satellite mission. During the expedition, a total of 30 Hereon Surface Drifters were deployed.
    Keywords: Changing Earth – Sustaining our Future; DATE/TIME; DEPTH, water; DRIFT; Drifter; Eastern South Atlantic; Energy Transfers in Atmosphere and Ocean; Helmholtz_ChangingEarth; LATITUDE; LONGITUDE; M188; M188_22-1; Meteor (1986); Sample code/label; SFB181; SONETT II
    Type: Dataset
    Format: text/tab-separated-values, 11464 data points
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  • 20
    Publication Date: 2024-06-27
    Description: The METEOR expedition M188 SONETT II, conducted in the southeast Atlantic, represents a collaborative initiative within the TRR181 framework. It brings together various observational projects with the goal of integrating diverse process studies to observe multiple energy compartments. This cruise coincided with the 'fast-sampling' (CalVal) phase of the Surface Water and Ocean Topography (SWOT) satellite mission. During the expedition, a total of 30 Hereon Surface Drifters were deployed.
    Keywords: Changing Earth – Sustaining our Future; DATE/TIME; DEPTH, water; DRIFT; Drifter; Eastern South Atlantic; Energy Transfers in Atmosphere and Ocean; Helmholtz_ChangingEarth; LATITUDE; LONGITUDE; M188; M188_9-1; Meteor (1986); Sample code/label; SFB181; SONETT II
    Type: Dataset
    Format: text/tab-separated-values, 32425 data points
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  • 21
    Publication Date: 2024-06-27
    Description: The METEOR expedition M188 SONETT II, conducted in the southeast Atlantic, represents a collaborative initiative within the TRR181 framework. It brings together various observational projects with the goal of integrating diverse process studies to observe multiple energy compartments. This cruise coincided with the 'fast-sampling' (CalVal) phase of the Surface Water and Ocean Topography (SWOT) satellite mission. During the expedition, a total of 30 Hereon Surface Drifters were deployed.
    Keywords: Changing Earth – Sustaining our Future; DATE/TIME; DEPTH, water; DRIFT; Drifter; Eastern South Atlantic; Energy Transfers in Atmosphere and Ocean; Helmholtz_ChangingEarth; LATITUDE; LONGITUDE; M188; M188_22-1; Meteor (1986); Sample code/label; SFB181; SONETT II
    Type: Dataset
    Format: text/tab-separated-values, 34275 data points
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  • 22
    Publication Date: 2024-06-27
    Description: The METEOR expedition M188 SONETT II, conducted in the southeast Atlantic, represents a collaborative initiative within the TRR181 framework. It brings together various observational projects with the goal of integrating diverse process studies to observe multiple energy compartments. This cruise coincided with the 'fast-sampling' (CalVal) phase of the Surface Water and Ocean Topography (SWOT) satellite mission. During the expedition, a total of 30 Hereon Surface Drifters were deployed.
    Keywords: Changing Earth – Sustaining our Future; DATE/TIME; DEPTH, water; DRIFT; Drifter; Eastern South Atlantic; Energy Transfers in Atmosphere and Ocean; Helmholtz_ChangingEarth; LATITUDE; LONGITUDE; M188; M188_9-1; Meteor (1986); Sample code/label; SFB181; SONETT II
    Type: Dataset
    Format: text/tab-separated-values, 33687 data points
    Location Call Number Expected Availability
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  • 23
    Publication Date: 2024-06-27
    Description: The METEOR expedition M188 SONETT II, conducted in the southeast Atlantic, represents a collaborative initiative within the TRR181 framework. It brings together various observational projects with the goal of integrating diverse process studies to observe multiple energy compartments. This cruise coincided with the 'fast-sampling' (CalVal) phase of the Surface Water and Ocean Topography (SWOT) satellite mission. During the expedition, a total of 30 Hereon Surface Drifters were deployed.
    Keywords: Changing Earth – Sustaining our Future; DATE/TIME; DEPTH, water; DRIFT; Drifter; Eastern South Atlantic; Energy Transfers in Atmosphere and Ocean; Helmholtz_ChangingEarth; LATITUDE; LONGITUDE; M188; M188_5-1; Meteor (1986); Sample code/label; SFB181; SONETT II
    Type: Dataset
    Format: text/tab-separated-values, 34778 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 24
    Publication Date: 2024-06-27
    Description: The METEOR expedition M188 SONETT II, conducted in the southeast Atlantic, represents a collaborative initiative within the TRR181 framework. It brings together various observational projects with the goal of integrating diverse process studies to observe multiple energy compartments. This cruise coincided with the 'fast-sampling' (CalVal) phase of the Surface Water and Ocean Topography (SWOT) satellite mission. During the expedition, a total of 30 Hereon Surface Drifters were deployed.
    Keywords: Changing Earth – Sustaining our Future; DATE/TIME; DEPTH, water; DRIFT; Drifter; Eastern South Atlantic; Energy Transfers in Atmosphere and Ocean; Helmholtz_ChangingEarth; LATITUDE; LONGITUDE; M188; M188_22-1; Meteor (1986); Sample code/label; SFB181; SONETT II
    Type: Dataset
    Format: text/tab-separated-values, 34961 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 25
    facet.materialart.
    Unknown
    PANGAEA
    In:  GEOMAR - Helmholtz Centre for Ocean Research Kiel
    Publication Date: 2024-06-27
    Description: Raw data acquired by position sensors on board RV METEOR during expedition M196 were processed to receive a validated master track which can be used as reference of further expedition data. During M196 the motion reference unit Kongsberg SeaTex AS MRU-5 combined with Kongsberg SeaTex AS Seapath 320 and two C and C Technologies GPS receivers C-NAV3050 were used as navigation sensors. Data were downloaded from DAVIS SHIP data base (https://dship.bsh.de) with a resolution of 1 sec. Processing and evaluation of the data is outlined in the data processing report. Processed data are provided as a master track with 1 sec resolution derived from the position sensors' data selected by priority and a generalized track with a reduced set of the most significant positions of the master track.
    Keywords: Calculated; Course; CT; DAM_Underway; DAM Underway Research Data; DATE/TIME; GoCW; LATITUDE; LONGITUDE; M196; M196-track; Meteor (1986); Speed; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 6330 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 26
    Publication Date: 2024-06-27
    Description: The METEOR expedition M188 SONETT II, conducted in the southeast Atlantic, represents a collaborative initiative within the TRR181 framework. It brings together various observational projects with the goal of integrating diverse process studies to observe multiple energy compartments. This cruise coincided with the 'fast-sampling' (CalVal) phase of the Surface Water and Ocean Topography (SWOT) satellite mission. During the expedition, a total of 30 Hereon Surface Drifters were deployed.
    Keywords: Changing Earth – Sustaining our Future; DATE/TIME; DEPTH, water; DRIFT; Drifter; Eastern South Atlantic; Energy Transfers in Atmosphere and Ocean; Helmholtz_ChangingEarth; LATITUDE; LONGITUDE; M188; M188_9-1; Meteor (1986); Sample code/label; SFB181; SONETT II
    Type: Dataset
    Format: text/tab-separated-values, 34494 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 27
    Publication Date: 2024-06-27
    Description: The METEOR expedition M188 SONETT II, conducted in the southeast Atlantic, represents a collaborative initiative within the TRR181 framework. It brings together various observational projects with the goal of integrating diverse process studies to observe multiple energy compartments. This cruise coincided with the 'fast-sampling' (CalVal) phase of the Surface Water and Ocean Topography (SWOT) satellite mission. During the expedition, a total of 30 Hereon Surface Drifters were deployed.
    Keywords: Changing Earth – Sustaining our Future; DATE/TIME; DEPTH, water; DRIFT; Drifter; Eastern South Atlantic; Energy Transfers in Atmosphere and Ocean; Helmholtz_ChangingEarth; LATITUDE; LONGITUDE; M188; M188_9-1; Meteor (1986); Sample code/label; SFB181; SONETT II
    Type: Dataset
    Format: text/tab-separated-values, 28687 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 28
    Publication Date: 2024-06-27
    Description: The METEOR expedition M188 SONETT II, conducted in the southeast Atlantic, represents a collaborative initiative within the TRR181 framework. It brings together various observational projects with the goal of integrating diverse process studies to observe multiple energy compartments. This cruise coincided with the 'fast-sampling' (CalVal) phase of the Surface Water and Ocean Topography (SWOT) satellite mission. During the expedition, a total of 30 Hereon Surface Drifters were deployed.
    Keywords: Changing Earth – Sustaining our Future; DATE/TIME; DEPTH, water; DRIFT; Drifter; Eastern South Atlantic; Energy Transfers in Atmosphere and Ocean; Helmholtz_ChangingEarth; LATITUDE; LONGITUDE; M188; M188_2-1; Meteor (1986); Sample code/label; SFB181; SONETT II
    Type: Dataset
    Format: text/tab-separated-values, 36833 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 29
    Publication Date: 2024-06-27
    Description: The METEOR expedition M188 SONETT II, conducted in the southeast Atlantic, represents a collaborative initiative within the TRR181 framework. It brings together various observational projects with the goal of integrating diverse process studies to observe multiple energy compartments. This cruise coincided with the 'fast-sampling' (CalVal) phase of the Surface Water and Ocean Topography (SWOT) satellite mission. During the expedition, a total of 30 Hereon Surface Drifters were deployed.
    Keywords: Changing Earth – Sustaining our Future; DATE/TIME; DEPTH, water; DRIFT; Drifter; Eastern South Atlantic; Energy Transfers in Atmosphere and Ocean; Helmholtz_ChangingEarth; LATITUDE; LONGITUDE; M188; M188_22-1; Meteor (1986); Sample code/label; SFB181; SONETT II
    Type: Dataset
    Format: text/tab-separated-values, 34300 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 30
    Publication Date: 2024-06-27
    Description: The METEOR expedition M188 SONETT II, conducted in the southeast Atlantic, represents a collaborative initiative within the TRR181 framework. It brings together various observational projects with the goal of integrating diverse process studies to observe multiple energy compartments. This cruise coincided with the 'fast-sampling' (CalVal) phase of the Surface Water and Ocean Topography (SWOT) satellite mission. During the expedition, a total of 30 Hereon Surface Drifters were deployed.
    Keywords: Changing Earth – Sustaining our Future; DATE/TIME; DEPTH, water; DRIFT; Drifter; Eastern South Atlantic; Energy Transfers in Atmosphere and Ocean; Helmholtz_ChangingEarth; LATITUDE; LONGITUDE; M188; M188_22-1; Meteor (1986); Sample code/label; SFB181; SONETT II
    Type: Dataset
    Format: text/tab-separated-values, 36591 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 31
    Publication Date: 2024-06-27
    Description: The METEOR expedition M188 SONETT II, conducted in the southeast Atlantic, represents a collaborative initiative within the TRR181 framework. It brings together various observational projects with the goal of integrating diverse process studies to observe multiple energy compartments. This cruise coincided with the 'fast-sampling' (CalVal) phase of the Surface Water and Ocean Topography (SWOT) satellite mission. During the expedition, a total of 30 Hereon Surface Drifters were deployed.
    Keywords: Changing Earth – Sustaining our Future; DATE/TIME; DEPTH, water; DRIFT; Drifter; Eastern South Atlantic; Energy Transfers in Atmosphere and Ocean; Helmholtz_ChangingEarth; LATITUDE; LONGITUDE; M188; M188_22-1; Meteor (1986); Sample code/label; SFB181; SONETT II
    Type: Dataset
    Format: text/tab-separated-values, 34350 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 32
    Publication Date: 2024-06-27
    Description: The METEOR expedition M188 SONETT II, conducted in the southeast Atlantic, represents a collaborative initiative within the TRR181 framework. It brings together various observational projects with the goal of integrating diverse process studies to observe multiple energy compartments. This cruise coincided with the 'fast-sampling' (CalVal) phase of the Surface Water and Ocean Topography (SWOT) satellite mission. During the expedition, a total of 30 Hereon Surface Drifters were deployed.
    Keywords: Changing Earth – Sustaining our Future; DATE/TIME; DEPTH, water; DRIFT; Drifter; Eastern South Atlantic; Energy Transfers in Atmosphere and Ocean; Helmholtz_ChangingEarth; LATITUDE; LONGITUDE; M188; M188_22-1; Meteor (1986); Sample code/label; SFB181; SONETT II
    Type: Dataset
    Format: text/tab-separated-values, 338 data points
    Location Call Number Expected Availability
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  • 33
    Publication Date: 2024-06-27
    Description: The METEOR expedition M188 SONETT II, conducted in the southeast Atlantic, represents a collaborative initiative within the TRR181 framework. It brings together various observational projects with the goal of integrating diverse process studies to observe multiple energy compartments. This cruise coincided with the 'fast-sampling' (CalVal) phase of the Surface Water and Ocean Topography (SWOT) satellite mission. During the expedition, a total of 30 Hereon Surface Drifters were deployed.
    Keywords: Changing Earth – Sustaining our Future; DATE/TIME; DEPTH, water; DRIFT; Drifter; Eastern South Atlantic; Energy Transfers in Atmosphere and Ocean; Helmholtz_ChangingEarth; LATITUDE; LONGITUDE; M188; M188_22-1; Meteor (1986); Sample code/label; SFB181; SONETT II
    Type: Dataset
    Format: text/tab-separated-values, 33750 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 34
    Publication Date: 2024-06-27
    Description: The METEOR expedition M188 SONETT II, conducted in the southeast Atlantic, represents a collaborative initiative within the TRR181 framework. It brings together various observational projects with the goal of integrating diverse process studies to observe multiple energy compartments. This cruise coincided with the 'fast-sampling' (CalVal) phase of the Surface Water and Ocean Topography (SWOT) satellite mission. During the expedition, a total of 30 Hereon Surface Drifters were deployed.
    Keywords: Changing Earth – Sustaining our Future; DATE/TIME; DEPTH, water; DRIFT; Drifter; Eastern South Atlantic; Energy Transfers in Atmosphere and Ocean; Helmholtz_ChangingEarth; LATITUDE; LONGITUDE; M188; M188_3-2; Meteor (1986); Sample code/label; SFB181; SONETT II
    Type: Dataset
    Format: text/tab-separated-values, 35738 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 35
    Publication Date: 2024-06-27
    Description: The METEOR expedition M188 SONETT II, conducted in the southeast Atlantic, represents a collaborative initiative within the TRR181 framework. It brings together various observational projects with the goal of integrating diverse process studies to observe multiple energy compartments. This cruise coincided with the 'fast-sampling' (CalVal) phase of the Surface Water and Ocean Topography (SWOT) satellite mission. During the expedition, a total of 30 Hereon Surface Drifters were deployed.
    Keywords: Changing Earth – Sustaining our Future; DATE/TIME; DEPTH, water; DRIFT; Drifter; Eastern South Atlantic; Energy Transfers in Atmosphere and Ocean; Helmholtz_ChangingEarth; LATITUDE; LONGITUDE; M188; M188_2-1; Meteor (1986); Sample code/label; SFB181; SONETT II
    Type: Dataset
    Format: text/tab-separated-values, 37257 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 36
    Publication Date: 2024-06-27
    Description: The METEOR expedition M188 SONETT II, conducted in the southeast Atlantic, represents a collaborative initiative within the TRR181 framework. It brings together various observational projects with the goal of integrating diverse process studies to observe multiple energy compartments. This cruise coincided with the 'fast-sampling' (CalVal) phase of the Surface Water and Ocean Topography (SWOT) satellite mission. During the expedition, a total of 30 Hereon Surface Drifters were deployed.
    Keywords: Changing Earth – Sustaining our Future; DATE/TIME; DEPTH, water; DRIFT; Drifter; Eastern South Atlantic; Energy Transfers in Atmosphere and Ocean; Helmholtz_ChangingEarth; LATITUDE; LONGITUDE; M188; M188_9-1; Meteor (1986); Sample code/label; SFB181; SONETT II
    Type: Dataset
    Format: text/tab-separated-values, 36966 data points
    Location Call Number Expected Availability
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  • 37
    facet.materialart.
    Unknown
    PANGAEA
    In:  Federal Institute for Geosciences and Natural Resources
    Publication Date: 2024-06-27
    Description: Raw data acquired by position sensors on board RV SONNE during expedition SO301 were processed to receive a validated master track which can be used as reference of further expedition data. During SO301 the motion reference unit Kongsberg SeaTex AS MRU-5 combined with Kongsberg SeaTex AS Seapath 320 and two GPS receivers SAAB MGL-4 were used as navigation sensors. Data were downloaded from DAVIS SHIP data base (https://dship.bsh.de) with a resolution of 1 sec. Processing and evaluation of the data is outlined in the data processing report. Processed data are provided as a master track with 1 sec resolution derived from the position sensors' data selected by priority and a generalized track with a reduced set of the most significant positions of the master track.
    Keywords: Calculated; Course; CT; DAM_Underway; DAM Underway Research Data; DATE/TIME; LATITUDE; LONGITUDE; SCIROCCO; SO301; SO301-track; Sonne_2; Speed; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 12376 data points
    Location Call Number Expected Availability
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  • 38
    Publication Date: 2024-06-27
    Description: The present dataset contains coccolithophores abundances (coccospheres/L). The samples were collected between Barcelona and the Ebro Delta (Western Mediterranean), during the MERS-BLUEISLAND cruise in November 2019, with rosette Niskin bottles investigating the photic zone (0-200 m). Quantitative analyses were performed using a polarized light microscope at 1000× magnification. Abundances were determined by counting at least 300 coccospheres per sample when possible. Coccosphere density and species relative abundances were calculated using the following formula: CD = (A × N)/(a × V) where A is the filtration area (mm2), N is the total number of coccospheres, a is the scanned area (mm2) and V is the volume of the filtered water (L). The Upper Photic Zone (UPZ) group includes Rhabdosphaera clavigera, Syracosphaera pulchra, Coronosphaera mediterranea, Umbellosphaera tenuis, Umbellosphaera spp., Discosphaera tubifera, Umbilicosphaera sibogae, Syracosphaera anthos, while Florisphaera profunda and Gladiolithus flabellatus were grouped as Lower Photic Zone (LPZ) taxa. The diversity of the total assemblage was estimated according to Harper (1999, doi:10.1017/S0016756800334410).
    Keywords: Acanthoica quattrospina; Alisphaera spp.; Anthosphaera robusta; Bottle, Niskin; Calcidiscus spp.; Calciosolenia brasiliensis; Calciosolenia murrayi; Calculated; Ceratolithus spp.; Coccolithophores; Coccoliths, lower photic zone taxa; Coccoliths, upper photic zone taxa; Coccosphere density; Coccospheres, density; Coronosphaera mediterranea; DATE/TIME; DEPTH, water; Discosphaera tubifera; Ebro River Delta; Elevation of event; Emiliania huxleyi; Evenness of species; Event label; Florisphaera profunda; Gephyrocapsa oceanica; Gephyrocapsa spp.; Gladiolithus flabellatus; Helicosphaera carteri; Helicosphaera spp.; Latitude of event; Light microscope, Zeiss [1000x magnification]; Living coccolithophores; Longitude of event; MERS-BLUEISLANDS_STD10; MERS-BLUEISLANDS_STD14; MERS-BLUEISLANDS_STD15; MERS-BLUEISLANDS_STD16; MERS-BLUEISLANDS_STD17; MERS-BLUEISLANDS_STD18; MERS-BLUEISLANDS_STD2; MERS-BLUEISLANDS_STD4; MERS-BLUEISLANDS_STD6; MERS-BLUEISLANDS_STD7; MERS-BLUEISLANDS_STD8; NIS; Observation; Pontosphaera spp.; Pontosphaera syracusana; Rhabdosphaera clavigera; Rhabdosphaera stylifera; Scyphosphaera apsteinii; Shannon Diversity Index; Species richness; Station label; Syracosphaera anthos; Syracosphaera pulchra; Syracosphaera sp.; Syracosphaera spp.; Umbellosphaera spp.; Umbellosphaera tenuis; Umbilicosphaera sibogae; Western Mediterranean Sea
    Type: Dataset
    Format: text/tab-separated-values, 2926 data points
    Location Call Number Expected Availability
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  • 39
    facet.materialart.
    Unknown
    PANGAEA
    In:  Federal Institute for Geosciences and Natural Resources
    Publication Date: 2024-06-27
    Description: Raw data acquired by position sensors on board RV SONNE during expedition SO301 were processed to receive a validated master track which can be used as reference of further expedition data. During SO301 the motion reference unit Kongsberg SeaTex AS MRU-5 combined with Kongsberg SeaTex AS Seapath 320 and two GPS receivers SAAB MGL-4 were used as navigation sensors. Data were downloaded from DAVIS SHIP data base (https://dship.bsh.de) with a resolution of 1 sec. Processing and evaluation of the data is outlined in the data processing report. Processed data are provided as a master track with 1 sec resolution derived from the position sensors' data selected by priority and a generalized track with a reduced set of the most significant positions of the master track.
    Keywords: 1 sec resolution; CT; DAM_Underway; DAM Underway Research Data; SCIROCCO; SO301; SO301-track; Sonne_2; Underway cruise track measurements
    Type: Dataset
    Format: application/zip, 159.3 MBytes
    Location Call Number Expected Availability
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  • 40
    Publication Date: 2024-06-27
    Description: The present dataset contains environmental variables: temperature, salinity, fluorescence, turbidity, nitrite, nitrate, phosphate, silicon dioxide, total alkalinity, dissolved inorganic carbon and pH. The samples were collected between Barcelona and the Ebro Delta (Western Mediterranean), during the MERS-BLUEISLAND cruise in November 2019, with rosette Niskin bottles equipped with CTD investigating the photic zone (0-200 m).
    Keywords: Alkalinity, total; Automatic potentiometric titrator, Methrom, Titrando 909; Bottle, Niskin; Calculated; Carbon, inorganic, dissolved; Chlorophyll fluorometer, Seapoint, Seapoint chlorophyll fluorometer; CTD, Sea-Bird, measured with conductivity sensor, SEA-BIRD, SBE4C; CTD, Sea-Bird, measured with temperature sensor, SEA-BIRD SBE 3Plus; CTD, Sea-Bird, measured with turbidity meter, SEA-BIRD, STM; DATE/TIME; DEPTH, water; Ebro River Delta; Elevation of event; Environmental variables; Event label; Fluorescence; Latitude of event; Longitude of event; MERS-BLUEISLANDS_STD10; MERS-BLUEISLANDS_STD14; MERS-BLUEISLANDS_STD15; MERS-BLUEISLANDS_STD16; MERS-BLUEISLANDS_STD17; MERS-BLUEISLANDS_STD18; MERS-BLUEISLANDS_STD2; MERS-BLUEISLANDS_STD4; MERS-BLUEISLANDS_STD6; MERS-BLUEISLANDS_STD7; MERS-BLUEISLANDS_STD8; NIS; Nitrate and Nitrite; Nitrite; Observation; pH; Phosphate; Salinity; Silicon dioxide; Spectrophotometer, Hach Lange GmbH, DR3900; Spectrophotometer Shimadzu UV-2600; Station label; Temperature, water; Turbidity (Nephelometric turbidity unit); VINDTA 3D system for Dissolved Inorganic Carbon measurement; Western Mediterranean Sea
    Type: Dataset
    Format: text/tab-separated-values, 1078 data points
    Location Call Number Expected Availability
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  • 41
    Publication Date: 2024-06-27
    Description: For petrographic analyses, point counting was used to quantitatively estimate the modal composition of sand and sandstones by totalling the occurrence of various mineral grains within a representative sample. The Gazzi-Dickinson methos was chosen for this study. A total of 80 cutting and core samples from IODP Expedition 348 were used for this study, covering a total depth transect from 1,140.5-3,000.5 mbsf of the Nankai Accretionary Prism (SW Japan) at sites C0002N and C0002P. All 80 samples were prepared for thin sections for quantitative modal compositional analysis at The Open University (United Kingdom). Samples were sieved to remove clay and silt from the unconsolidated material. Approximately 10 grams of sands were then separated from the sieved samples and mixed with epoxy. The epoxy grain mounts were sliced to thin section thickness, cemented to glass slides with epoxy resin, and then thin sections were completed in the usual method. Point-count analyses involved 400 points per sample. Each grain was assigned to a classification category (e.g., monocrystalline quartz, polycrystalline quartz, feldspar, volcanic lithic, sedimentary lithics, etc).
    Keywords: 348-C0002N; 348-C0002P; Chikyu; Clay minerals; Clinopyroxene; Counted; deep-marine sediments; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Event label; Exp348; Feldspar; Fossils; Latitude of event; Lithic grains, sedimentary; Lithic grains, volcanic; Longitude of event; Mica, grains; Minerals, accessory; Nankai Trough; Nannofossils; NanTroSEIZE Plate Boundary Drilling 3; Organic matter; petrography analysis; Quartz, monocrystalline; Quartz, polycrystalline; Sample code/label; Sample ID; zircon age dating
    Type: Dataset
    Format: text/tab-separated-values, 1200 data points
    Location Call Number Expected Availability
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  • 42
    Publication Date: 2024-06-27
    Description: The METEOR expedition M188 SONETT II, conducted in the southeast Atlantic, represents a collaborative initiative within the TRR181 framework. It brings together various observational projects with the goal of integrating diverse process studies to observe multiple energy compartments. This cruise coincided with the 'fast-sampling' (CalVal) phase of the Surface Water and Ocean Topography (SWOT) satellite mission. During the expedition, a total of 30 Hereon Surface Drifters were deployed.
    Keywords: Changing Earth – Sustaining our Future; DATE/TIME; DEPTH, water; DRIFT; Drifter; Eastern South Atlantic; Energy Transfers in Atmosphere and Ocean; Helmholtz_ChangingEarth; LATITUDE; LONGITUDE; M188; M188_22-1; Meteor (1986); Sample code/label; SFB181; SONETT II
    Type: Dataset
    Format: text/tab-separated-values, 38741 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 43
    Publication Date: 2024-06-27
    Description: The METEOR expedition M188 SONETT II, conducted in the southeast Atlantic, represents a collaborative initiative within the TRR181 framework. It brings together various observational projects with the goal of integrating diverse process studies to observe multiple energy compartments. This cruise coincided with the 'fast-sampling' (CalVal) phase of the Surface Water and Ocean Topography (SWOT) satellite mission. During the expedition, a total of 30 Hereon Surface Drifters were deployed.
    Keywords: Changing Earth – Sustaining our Future; DATE/TIME; DEPTH, water; DRIFT; Drifter; Eastern South Atlantic; Energy Transfers in Atmosphere and Ocean; Helmholtz_ChangingEarth; LATITUDE; LONGITUDE; M188; M188_4-1; Meteor (1986); Sample code/label; SFB181; SONETT II
    Type: Dataset
    Format: text/tab-separated-values, 35296 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 44
    Publication Date: 2024-06-27
    Description: The METEOR expedition M188 SONETT II, conducted in the southeast Atlantic, represents a collaborative initiative within the TRR181 framework. It brings together various observational projects with the goal of integrating diverse process studies to observe multiple energy compartments. This cruise coincided with the 'fast-sampling' (CalVal) phase of the Surface Water and Ocean Topography (SWOT) satellite mission. During the expedition, a total of 30 Hereon Surface Drifters were deployed.
    Keywords: Changing Earth – Sustaining our Future; DATE/TIME; DEPTH, water; DRIFT; Drifter; Eastern South Atlantic; Energy Transfers in Atmosphere and Ocean; Helmholtz_ChangingEarth; LATITUDE; LONGITUDE; M188; M188_5-1; Meteor (1986); Sample code/label; SFB181; SONETT II
    Type: Dataset
    Format: text/tab-separated-values, 31442 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 45
    Publication Date: 2024-06-27
    Description: The METEOR expedition M188 SONETT II, conducted in the southeast Atlantic, represents a collaborative initiative within the TRR181 framework. It brings together various observational projects with the goal of integrating diverse process studies to observe multiple energy compartments. This cruise coincided with the 'fast-sampling' (CalVal) phase of the Surface Water and Ocean Topography (SWOT) satellite mission. During the expedition, a total of 30 Hereon Surface Drifters were deployed.
    Keywords: Changing Earth – Sustaining our Future; DATE/TIME; DEPTH, water; DRIFT; Drifter; Eastern South Atlantic; Energy Transfers in Atmosphere and Ocean; Helmholtz_ChangingEarth; LATITUDE; LONGITUDE; M188; M188_2-2; Meteor (1986); Sample code/label; SFB181; SONETT II
    Type: Dataset
    Format: text/tab-separated-values, 13448 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 46
    Publication Date: 2024-06-27
    Description: The METEOR expedition M188 SONETT II, conducted in the southeast Atlantic, represents a collaborative initiative within the TRR181 framework. It brings together various observational projects with the goal of integrating diverse process studies to observe multiple energy compartments. This cruise coincided with the 'fast-sampling' (CalVal) phase of the Surface Water and Ocean Topography (SWOT) satellite mission. During the expedition, a total of 30 Hereon Surface Drifters were deployed.
    Keywords: Changing Earth – Sustaining our Future; DATE/TIME; DEPTH, water; DRIFT; Drifter; Eastern South Atlantic; Energy Transfers in Atmosphere and Ocean; Helmholtz_ChangingEarth; LATITUDE; LONGITUDE; M188; M188_9-1; Meteor (1986); Sample code/label; SFB181; SONETT II
    Type: Dataset
    Format: text/tab-separated-values, 37187 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 47
    Publication Date: 2024-06-27
    Description: The METEOR expedition M188 SONETT II, conducted in the southeast Atlantic, represents a collaborative initiative within the TRR181 framework. It brings together various observational projects with the goal of integrating diverse process studies to observe multiple energy compartments. This cruise coincided with the 'fast-sampling' (CalVal) phase of the Surface Water and Ocean Topography (SWOT) satellite mission. During the expedition, a total of 30 Hereon Surface Drifters were deployed.
    Keywords: Changing Earth – Sustaining our Future; DATE/TIME; DEPTH, water; DRIFT; Drifter; Eastern South Atlantic; Energy Transfers in Atmosphere and Ocean; Helmholtz_ChangingEarth; LATITUDE; LONGITUDE; M188; M188_22-1; Meteor (1986); Sample code/label; SFB181; SONETT II
    Type: Dataset
    Format: text/tab-separated-values, 34310 data points
    Location Call Number Expected Availability
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  • 48
    Publication Date: 2024-06-27
    Description: The METEOR expedition M188 SONETT II, conducted in the southeast Atlantic, represents a collaborative initiative within the TRR181 framework. It brings together various observational projects with the goal of integrating diverse process studies to observe multiple energy compartments. This cruise coincided with the 'fast-sampling' (CalVal) phase of the Surface Water and Ocean Topography (SWOT) satellite mission. During the expedition, a total of 30 Hereon Surface Drifters were deployed.
    Keywords: Changing Earth – Sustaining our Future; DATE/TIME; DEPTH, water; DRIFT; Drifter; Eastern South Atlantic; Energy Transfers in Atmosphere and Ocean; Helmholtz_ChangingEarth; LATITUDE; LONGITUDE; M188; M188_22-1; Meteor (1986); Sample code/label; SFB181; SONETT II
    Type: Dataset
    Format: text/tab-separated-values, 36057 data points
    Location Call Number Expected Availability
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  • 49
    Publication Date: 2024-06-27
    Description: The METEOR expedition M188 SONETT II, conducted in the southeast Atlantic, represents a collaborative initiative within the TRR181 framework. It brings together various observational projects with the goal of integrating diverse process studies to observe multiple energy compartments. This cruise coincided with the 'fast-sampling' (CalVal) phase of the Surface Water and Ocean Topography (SWOT) satellite mission. During the expedition, a total of 30 Hereon Surface Drifters were deployed.
    Keywords: Changing Earth – Sustaining our Future; DATE/TIME; DEPTH, water; DRIFT; Drifter; Eastern South Atlantic; Energy Transfers in Atmosphere and Ocean; Helmholtz_ChangingEarth; LATITUDE; LONGITUDE; M188; M188_4-1; Meteor (1986); Sample code/label; SFB181; SONETT II
    Type: Dataset
    Format: text/tab-separated-values, 36367 data points
    Location Call Number Expected Availability
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  • 50
    Publication Date: 2024-06-27
    Description: The METEOR expedition M188 SONETT II, conducted in the southeast Atlantic, represents a collaborative initiative within the TRR181 framework. It brings together various observational projects with the goal of integrating diverse process studies to observe multiple energy compartments. This cruise coincided with the 'fast-sampling' (CalVal) phase of the Surface Water and Ocean Topography (SWOT) satellite mission. During the expedition, a total of 30 Hereon Surface Drifters were deployed.
    Keywords: Changing Earth – Sustaining our Future; Energy Transfers in Atmosphere and Ocean; Helmholtz_ChangingEarth; SFB181
    Type: Dataset
    Format: application/zip, 30 datasets
    Location Call Number Expected Availability
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  • 51
    Publication Date: 2024-06-27
    Description: The dataset represents the number, the total and the standardized biomass (catch per unit effort) of 94 deep-pelagic fish species collected by pelagic trawling in submarine canyons of the Bay of Biscay slope during the EVHOE scientific cruises on R/V Thalassa in autumn between 2002 and 2019 (https://doi.org/10.18142/8). Fifty-six trawls were conducted at night between 20 m and 2000 m depth. The trawl net was 192 m long with a headline of 76 m and a foot rope of 70 m. The average vertical mean mouth opening was about 24 m and the horizontal opening of about 58 m. The mesh size gradually decreases from very large 8 m meshes at the mouth to 20 mm meshes in the codend. To allow the capture of very small specimens, the trawl is also equipped with a 7.5 m long sock with a 12 mm mesh. The trawl had an average vertical mouth opening of 24 m and a horizontal opening of 58 m. The duration of the haul was 1 hour at 4 kn. The trawl did not have an opening-closing mechanism. Therefore, some individuals might have been caught during the descent and ascent of the gear, however a higher trawl speed on deployment and a low speed on retrieval were implemented to reduce bycatch at shallower depths than the target depth. The biomass per unit effort is standardized by the volume hauled and was calculated by multiplying the vertical and horizontal trawl opening and the distance trawled. Individuals were identified by expert ichthyologists to the species level whenever possible, otherwise they were identified to the genus or family level, especially when individuals were too small or damaged. Species or taxa were counted and most often weighed. When weighing was not possible, an estimate of the average weight of individuals over the whole time series was calculated and the total weight per species was estimated.
    Keywords: Anoplogaster cornuta; Anoplogaster cornuta, biomass, wet mass; Anoplogaster cornuta, mass; Arctozenus risso; Arctozenus risso, biomass, wet mass; Arctozenus risso, mass; Argyropelecus hemigymnus; Argyropelecus hemigymnus, biomass, wet mass; Argyropelecus hemigymnus, mass; Argyropelecus olfersii; Argyropelecus olfersii, biomass, wet mass; Argyropelecus olfersii, mass; Astronesthes niger; Astronesthes niger, biomass, wet mass; Astronesthes niger, mass; Avocettina infans; Avocettina infans, biomass, wet mass; Avocettina infans, mass; Barbantus curvifrons; Barbantus curvifrons, biomass, wet mass; Barbantus curvifrons, mass; Bathylagichthys greyae; Bathylagichthys greyae, biomass, wet mass; Bathylagichthys greyae, mass; Bathylagus euryops; Bathylagus euryops, biomass, wet mass; Bathylagus euryops, mass; Bathylagus spp.; Bathylagus spp., biomass, wet mass; Bathylagus spp., mass; Bay of Biscay; Benthosema glaciale; Benthosema glaciale, biomass, wet mass; Benthosema glaciale, mass; Beryx splendens; Beryx splendens, biomass, wet mass; Beryx splendens, mass; Bolinichthys indicus; Bolinichthys indicus, biomass, wet mass; Bolinichthys indicus, mass; Bolinichthys supralateralis; Bolinichthys supralateralis, biomass, wet mass; Bolinichthys supralateralis, mass; Borostomias antarcticus; Borostomias antarcticus, biomass, wet mass; Borostomias antarcticus, mass; Calculated; Ceratoscopelus maderensis; Ceratoscopelus maderensis, biomass, wet mass; Ceratoscopelus maderensis, mass; Chauliodus sloani; Chauliodus sloani, biomass, wet mass; Chauliodus sloani, mass; Counted; Cyclothone spp.; Cyclothone spp., biomass, wet mass; Cyclothone spp., mass; Date/Time of event; Date/Time of event 2; DEPTH, water; Derichthys serpentinus; Derichthys serpentinus, biomass, wet mass; Derichthys serpentinus, mass; Derichthys spp.; Derichthys spp., biomass, wet mass; Derichthys spp., mass; Diaphus dumerilii; Diaphus dumerilii, biomass, wet mass; Diaphus dumerilii, mass; Diaphus metopoclampus; Diaphus metopoclampus, biomass, wet mass; Diaphus metopoclampus, mass; Diaphus mollis; Diaphus mollis, biomass, wet mass; Diaphus mollis, mass; Diaphus spp.; Diaphus spp., biomass, wet mass; Diaphus spp., mass; Dolicholagus longirostris; Dolicholagus longirostris, biomass, wet mass; Dolicholagus longirostris, mass; Dolichopteryx longipes; Dolichopteryx longipes, biomass, wet mass; Dolichopteryx longipes, mass; Electrona risso; Electrona risso, biomass, wet mass; Electrona risso, mass; Entelurus aequoreus; Entelurus aequoreus, biomass, wet mass; Entelurus aequoreus, mass; Eurypharynx pelecanoides; Eurypharynx pelecanoides, biomass, wet mass; Eurypharynx pelecanoides, mass; Event label; Evermannella balbo; Evermannella balbo, biomass, wet mass; Evermannella balbo, mass; EVHOE-2002; EVHOE-2003; EVHOE-2007; EVHOE-2008; EVHOE-2010; EVHOE-2011; EVHOE-2016; EVHOE-2017; EVHOE-2018; EVHOE-2019; EVHOE-G0344; EVHOE-G0349; EVHOE-G0354; EVHOE-G0365; EVHOE-G0370; EVHOE-G0380; EVHOE-G0399; EVHOE-H0400; EVHOE-H0411; EVHOE-H0419; EVHOE-H0425; EVHOE-H0431; EVHOE-H0467; EVHOE-L0731; EVHOE-L0736; EVHOE-L0742; EVHOE-L0747; EVHOE-L0752; EVHOE-L0761; EVHOE-L0766; EVHOE-M0855; EVHOE-M0862; EVHOE-M0876; EVHOE-M0881; EVHOE-M0887; EVHOE-M0892; EVHOE-O0959; EVHOE-O0964; EVHOE-O0969; EVHOE-O0978; EVHOE-O0983; EVHOE-O0995; EVHOE-P1048; EVHOE-P1053; EVHOE-P1062; EVHOE-P1067; EVHOE-P1072; EVHOE-U0508; EVHOE-U0514; EVHOE-U0519; EVHOE-U0524; EVHOE-U0530; EVHOE-U0536; EVHOE-U0541; EVHOE-V0494; EVHOE-W0534; EVHOE-W0545; EVHOE-W0551; EVHOE-W0562; EVHOE-W0568; EVHOE-X0447; EVHOE-X0453; EVHOE-X0458; EVHOE-X0464; EVHOE-X0470; EVHOE-X0476; Gadiculus argenteus; Gadiculus argenteus, biomass, wet mass; Gadiculus argenteus, mass; Gonostoma elongatum; Gonostoma elongatum, biomass, wet mass; Gonostoma elongatum, mass; GOV36-47; Grande Ouverture Verticale 36/47; Holtbyrnia anomala; Holtbyrnia anomala, biomass, wet mass; Holtbyrnia anomala, mass; Holtbyrnia macrops; Holtbyrnia macrops, biomass, wet mass; Holtbyrnia macrops, mass; Howella atlantica; Howella atlantica, biomass, wet mass; Howella atlantica, mass; Lampadena atlantica; Lampadena atlantica, biomass, wet mass; Lampadena atlantica, mass; Lampadena speculigera; Lampadena speculigera, biomass, wet mass; Lampadena speculigera, mass; Lampadena urophaos; Lampadena urophaos, biomass, wet mass; Lampadena urophaos, mass; Lampanyctus crocodilus; Lampanyctus crocodilus, biomass, wet mass; Lampanyctus crocodilus, mass; Lampanyctus festivus; Lampanyctus festivus, biomass, wet mass; Lampanyctus festivus, mass; Lampanyctus macdonaldi; Lampanyctus macdonaldi, biomass, wet mass; Lampanyctus macdonaldi, mass; Lampanyctus spp.; Lampanyctus spp., biomass, wet mass; Lampanyctus spp., mass; Latitude of event; Latitude of event 2; Leptostomias gladiator; Leptostomias gladiator, biomass, wet mass; Leptostomias gladiator, mass; Lestidiops affinis; Lestidiops affinis, biomass, wet mass; Lestidiops affinis, mass; Lestidiops sphyrenoides; Lestidiops sphyrenoides, biomass, wet mass; Lestidiops sphyrenoides, mass; Lobianchia gemellarii; Lobianchia gemellarii, biomass, wet mass; Lobianchia gemellarii, mass; Longitude of event; Longitude of event 2; Lyconus brachycolus; Lyconus brachycolus, biomass, wet mass; Lyconus brachycolus, mass; Macroparalepis affinis; Macroparalepis affinis, biomass, wet mass; Macroparalepis affinis, mass; Magnisudis atlantica; Magnisudis atlantica, biomass, wet mass; Magnisudis atlantica, mass; Malacosteus niger; Malacosteus niger, biomass, wet mass; Malacosteus niger, mass; Maulisia argipalla; Maulisia argipalla, biomass, wet mass; Maulisia argipalla, mass; Maulisia mauli; Maulisia mauli, biomass, wet mass; Maulisia mauli, mass; Maulisia microlepis; Maulisia microlepis, biomass, wet mass; Maulisia microlepis, mass; Maurolicus muelleri; Maurolicus muelleri, biomass, wet mass; Maurolicus muelleri, mass; Melanolagus bericoides; Melanolagus bericoides, biomass, wet mass; Melanolagus bericoides, mass; Melanonus zugmayeri; Melanonus zugmayeri, biomass, wet mass; Melanonus zugmayeri, mass; Melanostigma atlanticum; Melanostigma atlanticum, biomass, wet mass; Melanostigma atlanticum, mass; Melanostomias bartonbeani; Melanostomias bartonbeani, biomass, wet mass; Melanostomias bartonbeani, mass; Mentodus rostratus; Mentodus rostratus, biomass, wet mass; Mentodus rostratus, mass; Myctophidae; Myctophidae, biomass, wet mass; Myctophidae, mass; Myctophum punctatum; Myctophum punctatum, biomass, wet mass; Myctophum punctatum, mass; Nannobrachium atrum; Nannobrachium atrum, biomass, wet mass; Nannobrachium atrum, mass; Nannobrachium spp.; Nannobrachium spp., biomass, wet mass; Nannobrachium spp., mass; Nansenia oblita; Nansenia oblita, biomass, wet mass; Nansenia oblita, mass; Nansenia spp.; Nansenia spp., biomass, wet mass; Nansenia spp., mass; Neonesthes capensis; Neonesthes capensis, biomass, wet mass; Neonesthes capensis, mass; Nessorhamphus ingolfianus; Nessorhamphus ingolfianus, biomass, wet mass; Nessorhamphus ingolfianus, mass; Normichthys operosus; Normichthys operosus, biomass, wet mass; Normichthys operosus, mass; Notoscopelus kroyeri; Notoscopelus kroyeri, biomass, wet mass; Notoscopelus kroyeri, mass; Oneirodes anisacanthus; Oneirodes anisacanthus, biomass, wet mass; Oneirodes anisacanthus, mass; Oneirodes carlsbergi; Oneirodes carlsbergi, biomass, wet mass; Oneirodes carlsbergi, mass; Parabrotulidae; Parabrotulidae, biomass, wet mass; Parabrotulidae, mass; Paralepis coregonoides; Paralepis coregonoides, biomass, wet mass; Paralepis coregonoides, mass; Photostomias guernei; Photostomias guernei, biomass, wet mass; Photostomias guernei, mass; Photostylus pycnopterus; Photostylus pycnopterus, biomass, wet mass; Photostylus pycnopterus, mass; Platytroctidae; Platytroctidae, biomass, wet mass; Platytroctidae, mass; Polymetme thaeocoryla; Polymetme thaeocoryla, biomass, wet mass; Polymetme thaeocoryla, mass; Poromitra megalops; Poromitra megalops, biomass, wet mass; Poromitra megalops, mass;
    Type: Dataset
    Format: text/tab-separated-values, 15822 data points
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  • 52
    Publication Date: 2024-06-27
    Description: Raw multibeam bathymetry data were collected aboard RV METEOR during cruise M189 using a Kongsberg EM 122 multibeam echosounder. The expedition took place during 16.04.2023-13.05.2023 from Walvis Bay to Walvis Bay (Namibia) in the Central and Southern Atlantic Ocean. The main objective of M189 was to measure the variability of the circulation and the coastal upwelling off Angola and Namibia. Data were recorded within the Namibia and Angola EEZ. Sound velocity profiles (SVP) were applied on the data for calibration. Please see environmental data and the cruise report for details. The data are unprocessed and can therefore contain incorrect depth measurements (artifacts) if not further processed. Note that refraction errors may occur when no proper SVP is applied. Acquisition and provision of the data are part of the DAM Underway Project and published according to the FAIR principles.
    Keywords: BANINO; Bathymetry; Binary Object; Binary Object (File Size); Binary Object (Media Type); Comment; DAM_Underway; DAM Underway Research Data; Data file recording distance; Data file recording duration; DATE/TIME; ELEVATION; EM122; EM122 multibeam echosounder; Event label; Extracted from file; Extracted with MB-System; File content; Kongsberg datagram raw file name; LATITUDE; LONGITUDE; M189; M189_0_Underway-3; Meteor (1986); Multibeam Echosounder; Number of pings; Ship speed; Start of data file, depth; Start of data file, heading; Start of data file recording, date/time; Start of data file recording, latitude; Start of data file recording, longitude; Stop of data file, depth; Stop of data file, heading; Stop of data file recording, date/time; Stop of data file recording, latitude; Stop of data file recording, longitude
    Type: Dataset
    Format: text/tab-separated-values, 17814 data points
    Location Call Number Expected Availability
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  • 53
    Publication Date: 2024-06-27
    Description: Passive acoustic monitoring (PAM) data were collected by recorder SV1025 of type Sono.Vault (manufactured by develogic GmbH, Hamburg, Germany) at 59.0438° S, 0.082° E, mooring AWI227-12, in Weddell Sea, Atlantic sector of the Southern Ocean. During a deployment period from December 2012 to December 2014, passive acoustic data were collected from December 2012 to July 2013 (recording period) by SV1025 as part of the Hybrid Antarctic Float Observing System (HAFOS) in the Weddell Sea. The recorder was moored at 1020 m depth and scheduled to record continuously at a sample rate of 5,333 Hz. Further details about the data acquisition and processing of this data set can be found in the accompanying metadata file (see Additional metadata) as well as the data processing report (see Data Processing Report). Passive acoustic data archived here represent data processing Level 2+ (see the associated data processing report), deviating from Standard Operation Procedure (SOP) Glossary (Thomisch et al. 2023a). Further information on data processing with regard to data preparation and standardization can be found in the associated SOP Part 1: Data preparation and standardization (Thomisch et al. 2023b).
    Keywords: ANT-XXIX/2; ANT-XXX/2; Audio file; Audio file (File Size); AWI227-12; DATE/TIME; DEPTH, water; HAFOS; Hybrid Antarctic Float Observation System; MOOR; Mooring; Mooring (long time); MOORY; Passive acoustic recorder Sono.Vault, develogic GmbH; Polarstern; PS81; PS81/039-3; PS89; PS89/020-1; South Atlantic Ocean
    Type: Dataset
    Format: text/tab-separated-values, 214 data points
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  • 54
    Publication Date: 2024-06-27
    Description: Passive acoustic monitoring (PAM) data were collected by recorder AU0085 of type AURAL (Autonomous Underwater Recorder for Acoustic Listening (AURAL; Model 2, Multi-Électronique) at 66.0188° S, 0.0795° E, mooring AWI230-6, in the Weddell Sea, Atlantic sector of the Southern Ocean. Passive acoustic data were collected from March 2008 to December 2010 by AU0085 as part of the Hybrid Antarctic Float Observing System (HAFOS) in the Weddell Sea. The recorder was moored at 189 m depth and scheduled to record at a duty cycle of 5 min per 4 h at a sample rate of 32,768 Hz. Further details about the data acquisition and processing of this data set can be found in the accompanying metadata file (see Additional metadata) as well as the data processing report (see Data Processing Report). Passive acoustic data archived here represent data processing Level 1+, according to the standards defined in the associated Standard Operation Procedure (SOP) Glossary (Thomisch et al. 2023a). Further information on data processing with regard to data preparation and standardization can be found in the associated SOP Part 1: Data preparation and standardization (Thomisch et al. 2023b).
    Keywords: ANT-XXIV/3; ANT-XXVII/2; Audio file; Audio file (File Size); Autonomous Underwater Recorder for Acoustic Listening, Multi-Électronique, AURAL Model 2; AWI230-06,AWI230-6; AWI230-6; AWI230-6,AWI230-06; DATE/TIME; DEPTH, water; HAFOS; Hybrid Antarctic Float Observation System; Lazarev Sea; MOOR; Mooring; Mooring (long time); MOORY; Polarstern; PS71; PS71/159-3; PS77; PS77/058-1; Weddell Sea
    Type: Dataset
    Format: text/tab-separated-values, 1014 data points
    Location Call Number Expected Availability
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  • 55
    Publication Date: 2024-06-27
    Description: Passive acoustic monitoring (PAM) data were collected by recorder AU0086 of type AURAL (Autonomous Underwater Recorder for Acoustic Listening (AURAL; Model 2, Multi-Électronique) at 68.9957° S, 0.0028° E, mooring AWI232-9, in the Weddell Sea, Atlantic sector of the Southern Ocean. Passive acoustic data were collected from March 2008 to December 2010 by AU0086 as part of the Hybrid Antarctic Float Observing System (HAFOS) in the Weddell Sea. The recorder was moored at 206 m depth and scheduled to record at a duty cycle of 5 min per 4 h at a sample rate of 32,768 Hz. Further details about the data acquisition and processing of this data set can be found in the accompanying metadata file (see Additional metadata) as well as the data processing report (see Data Processing Report). Passive acoustic data archived here represent data processing Level 1+, according to the standards defined in the associated Standard Operation Procedure (SOP) Glossary (Thomisch et al. 2023a). Further information on data processing with regard to data preparation and standardization can be found in the associated SOP Part 1: Data preparation and standardization (Thomisch et al. 2023b).
    Keywords: ANT-XXIV/3; ANT-XXVII/2; Audio file; Audio file (File Size); Autonomous Underwater Recorder for Acoustic Listening, Multi-Électronique, AURAL Model 2; AWI232-9; AWI232-9,AWI232-09; DATE/TIME; DEPTH, water; HAFOS; Hybrid Antarctic Float Observation System; MOOR; Mooring; Mooring (long time); MOORY; Polarstern; PS71; PS71/175-4; PS77; PS77/066-2; Weddell Sea
    Type: Dataset
    Format: text/tab-separated-values, 1014 data points
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  • 56
    Publication Date: 2024-06-27
    Description: Passive acoustic monitoring (PAM) data were collected by recorder AU0231 of type AURAL (Autonomous Underwater Recorder for Acoustic Listening (AURAL; Model 2, Multi-Électronique) at 61.0147° S, 55.9755° W, mooring AWI251-1, in the Weddell Sea, Atlantic sector of the Southern Ocean. Passive acoustic data were collected from January 2013 to February 2016 by AU0231 as part of the Hybrid Antarctic Float Observing System (HAFOS) in the Weddell Sea. The recorder was moored at 210 m depth and scheduled to record at a duty cycle of 5 min per hour at a sample rate of 32,768 Hz. Further details about the data acquisition and processing of this data set can be found in the accompanying metadata file (see Additional metadata) as well as the data processing report (see Data Processing Report). Passive acoustic data archived here represent data processing Level 1+, according to the standards defined in the associated Standard Operation Procedure (SOP) Glossary (Thomisch et al. 2023a). Further information on data processing with regard to data preparation and standardization can be found in the associated SOP Part 1: Data preparation and standardization (Thomisch et al. 2023b).
    Keywords: ANT-XXIX/2; ANT-XXXI/2 FROSN; Audio file; Autonomous Underwater Recorder for Acoustic Listening, Multi-Électronique, AURAL Model 2; AWI251-1,AWI251-01; DATE/TIME; DEPTH, water; HAFOS; Hybrid Antarctic Float Observation System; MOOR; Mooring; Polarstern; PS81; PS81/112-1; PS96; PS96/118-1; Scotia Sea; Weddell Sea
    Type: Dataset
    Format: text/tab-separated-values, 1121 data points
    Location Call Number Expected Availability
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  • 57
    Publication Date: 2024-06-27
    Description: Aerobic Anoxygenic Phototrophic (AAP) bacteria are an important component of freshwater bacterioplankton. They can support their heterotrophic metabolism with energy from light, and by that enhance their growth efficiency. Based on results from cultures, it was hypothesized that photoheterotrophy provides an advantage under carbon limitation and facilitates access to recalcitrant or low-energy carbon sources. However, verification of these hypotheses for natural AAP communities has been lacking. Here, we conducted whole community manipulation experiments and compared the growth of AAP bacteria under carbon limited and with recalcitrant (lignin) or low energy (acetate) carbon sources under dark and infra-red (IR) light conditions to elucidate how they profit from photoheterotrophy. We performed two whole community manipulation experiments in 2-litre microcosms. The first experiment was conducted in June 2018. Lignin was used as the recalcitrant carbon source. Samples were collected every 12 hours. The second experiment was conducted in October 2018. Acetate was used as the low-energy carbon source. Samples were collected every 24 hours. Both experiments were done in at in situ temperature. We measured concentrations of bacteriochlorophyll-a, total prokaryotic count, aerobic anoxygenic phototrophic bacteria count, and heterotrophic nanoflagellates count. This dataset is related to Piwosz et al. (in prep).
    Keywords: Bacteria, aerobic, anoxygenic, phototrophic; Bacteriochlorophyll a; Date/time start, experiment; Duration; Experimental condition; Fluorometer, PSI (Photon Systems Instruments), spol. s.r.o., FL200/PS; Ingoranic basal medium dilution according to Hahn et al. (20023); Mercury thermometer; Microscope, Carl Zeiss, Axio Imager.D2; coupled with Collibri LED module illumination system, Carl Zeiss; Nanoflagellates, heterotrophic; Prokaryotes; Replicate; Sample code/label; Treatment: light condition; Treatment: temperature; Type of study
    Type: Dataset
    Format: text/tab-separated-values, 2156 data points
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  • 58
    Publication Date: 2024-06-27
    Description: The METEOR expedition M188 SONETT II, conducted in the southeast Atlantic, represents a collaborative initiative within the TRR181 framework. It brings together various observational projects with the goal of integrating diverse process studies to observe multiple energy compartments. This cruise coincided with the 'fast-sampling' (CalVal) phase of the Surface Water and Ocean Topography (SWOT) satellite mission. During the expedition, a total of 30 Hereon Surface Drifters were deployed.
    Keywords: Changing Earth – Sustaining our Future; DATE/TIME; DEPTH, water; DRIFT; Drifter; Eastern South Atlantic; Energy Transfers in Atmosphere and Ocean; Helmholtz_ChangingEarth; LATITUDE; LONGITUDE; M188; M188_4-1; Meteor (1986); Sample code/label; SFB181; SONETT II
    Type: Dataset
    Format: text/tab-separated-values, 34367 data points
    Location Call Number Expected Availability
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  • 59
    Publication Date: 2024-06-27
    Description: The METEOR expedition M188 SONETT II, conducted in the southeast Atlantic, represents a collaborative initiative within the TRR181 framework. It brings together various observational projects with the goal of integrating diverse process studies to observe multiple energy compartments. This cruise coincided with the 'fast-sampling' (CalVal) phase of the Surface Water and Ocean Topography (SWOT) satellite mission. During the expedition, a total of 30 Hereon Surface Drifters were deployed.
    Keywords: Changing Earth – Sustaining our Future; DATE/TIME; DEPTH, water; DRIFT; Drifter; Eastern South Atlantic; Energy Transfers in Atmosphere and Ocean; Helmholtz_ChangingEarth; LATITUDE; LONGITUDE; M188; M188_3-1; Meteor (1986); Sample code/label; SFB181; SONETT II
    Type: Dataset
    Format: text/tab-separated-values, 34149 data points
    Location Call Number Expected Availability
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  • 60
    Publication Date: 2024-06-27
    Description: The METEOR expedition M188 SONETT II, conducted in the southeast Atlantic, represents a collaborative initiative within the TRR181 framework. It brings together various observational projects with the goal of integrating diverse process studies to observe multiple energy compartments. This cruise coincided with the 'fast-sampling' (CalVal) phase of the Surface Water and Ocean Topography (SWOT) satellite mission. During the expedition, a total of 30 Hereon Surface Drifters were deployed.
    Keywords: Changing Earth – Sustaining our Future; DATE/TIME; DEPTH, water; DRIFT; Drifter; Eastern South Atlantic; Energy Transfers in Atmosphere and Ocean; Helmholtz_ChangingEarth; LATITUDE; LONGITUDE; M188; M188_22-1; Meteor (1986); Sample code/label; SFB181; SONETT II
    Type: Dataset
    Format: text/tab-separated-values, 35163 data points
    Location Call Number Expected Availability
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  • 61
    Publication Date: 2024-06-27
    Description: The METEOR expedition M188 SONETT II, conducted in the southeast Atlantic, represents a collaborative initiative within the TRR181 framework. It brings together various observational projects with the goal of integrating diverse process studies to observe multiple energy compartments. This cruise coincided with the 'fast-sampling' (CalVal) phase of the Surface Water and Ocean Topography (SWOT) satellite mission. During the expedition, a total of 30 Hereon Surface Drifters were deployed.
    Keywords: Changing Earth – Sustaining our Future; DATE/TIME; DEPTH, water; DRIFT; Drifter; Eastern South Atlantic; Energy Transfers in Atmosphere and Ocean; Helmholtz_ChangingEarth; LATITUDE; LONGITUDE; M188; M188_5-1; Meteor (1986); Sample code/label; SFB181; SONETT II
    Type: Dataset
    Format: text/tab-separated-values, 35265 data points
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  • 62
    Publication Date: 2024-06-27
    Description: Abstract
    Description: The data comprises time series from three automatic meteorological and snow-hydrological stations situated in the Rofental (1891–3772 m a.s.l., Ötztal Alps, Austria). The recordings have been collected from Jan 2017 to Aug 2023. Some data sets represent continuations of time series at existing locations, others come from new installations complementing the scientific monitoring infrastructure in the research catchment. The stations are situated at 2737, 2805, and 2919 m a.s.l. and include automatic measurements of meteorological (temperature, precipitation, humidity, wind speed, and radiation fluxes) and snow-hydrological variables (snow depth, snow water equivalent, volumetric solid and liquid water content, snow density, layered snow temperature profiles, snow surface temperature, and snow drift). The data are sampled by fully automatic weather stations (AWS). The data retrieved by the sensors is stored on a logger in 10 min. temporal resolution. The data is continuously transferred by GSM to a server. The data processing consists of transfer of the raw data from the logger to a data server, basic processing steps (e.g., temperature correction long-wave radiation, decumulating precipitation measurements), and a semi-automatic correction for erroneous values.
    Keywords: meteorological stations ; snow-hydrological measurements ; Alpine catchment ; EARTH SCIENCE 〉 ATMOSPHERE ; EARTH SCIENCE 〉 CRYOSPHERE 〉 SNOW/ICE ; EARTH SCIENCE 〉 TERRESTRIAL HYDROSPHERE 〉 SNOW/ICE ; In Situ/Laboratory Instruments
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  • 63
    Publication Date: 2024-06-27
    Description: Neues Konzept soll den Meeresschutz in Kiel voranbringen - Expertin Nicole Walter erläutert die Grundzüge - Mitmach-Angebot am Samstag
    Type: Newspaper report , NonPeerReviewed
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  • 64
    Publication Date: 2024-06-27
    Description: Ob Delfine, Seepferdchen oder Schildkröten - in Nord- und Ostsee tummeln sich außergewöhnliche Meeresgäste
    Type: Newspaper report , NonPeerReviewed
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  • 65
    Publication Date: 2024-06-27
    Description: 20 Jahre nach der ersten Planungsidee: Geomar-'- Neubau am Seefischmarkt in Wellingdorf eingeweiht
    Type: Newspaper report , NonPeerReviewed
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  • 66
    Publication Date: 2024-06-27
    Description: Highlights • New geophysical data and samples redefine submarine volcanism in Sicilian Channel. • Three dominant bands of volcanism are distinguished. • Ancient, eroded structures aligned at 120° are tied to faulted banks in the north. • Younger band of similarly aligned volcanism in the south is linked to grabens. • Youngest structures comprise small, dispersed volcanoes with distinct orientation. Abstract The origin and role of volcanism in continental rifts remains poorly understood in comparison to other volcano-tectonic settings. The Sicilian Channel (central Mediterranean Sea) is largely floored by continental crust and represents an area affected by pronounced crustal extension and strike-slip tectonism. It hosts a variety of volcanic landforms closely associated with faults, which can be used to better understand the nature and distribution of rift-related volcanism. A paucity of appropriate seafloor data in the Sicilian Channel has led to uncertainties regarding the location, volume, sources and timing of submarine volcanism. To improve on this situation, we use newly acquired geophysical data (multibeam echosounder and magnetic data, sub-bottom profiles) and dredged seafloor samples to: (i) re-assess the evidence for submarine volcanism in the Sicilian Channel and define its spatial pattern, (ii) infer the relative age and style of magmatism, and (iii) relate this to the dominant tectonic structures in the region. Quaternary rift-related volcanism has been focused at Pantelleria and Linosa, at the northwest boundaries of their respective NW-SE trending grabens. Subsidiary and older volcanic sites potentially occur at the Linosa III and Pantelleria SE seamounts, collectively representing the only sites of recent volcanism that can be directly related to the main rift process. These long-lived polygenetic volcanic landforms have been shaped by magmatism that is directly correlated with extensional faulting and buried igneous bodies. Older volcanic landforms, sharing a similar scale and alignment, occur to the north at Nameless Bank and Adventure Bank. These deeply eroded volcanoes have likely been inactive since the Pliocene and are probably related to earlier stages of crustal thinning and underlying feeder structures in the northern region of the Sicilian Channel. Along a similar alignment, Pinne Bank, SE Pinne Bank and Cimotoe in the northern Sicilian Channel lack a surface volcanic signature but are associated with intrusive bodies or deeply buried volcanic rock masses. Terrible Bank, in the same region, also shows evidence of ancient, polygenetic magmatism, but was subject to significant erosion and lacks a prominent alignment. The much younger volcanism at Graham Volcanic Field and along the northern Capo-Granitola-Sciacca Fault Zone differs markedly from that observed in the other study areas. Here, the low-volume and scattered volcanic activity is driven by shallow-water mafic magma eruptions, which gave rise to small individual cones. These sites are associated with large fault structures away from the main rift axis and may have a distinct magmatic origin. Dispersed active fluid venting occurs across both ancient and young volcanic sites in the region and is directly associated with shallow magmatic bodies within tectonically-controlled basins. Our study provides the foundation for an updated tectonic and magmatic framework for the Sicilian Channel, and for future detailed chronological and geochemical assessment of the sources and evolution of magmatic processes in the region.
    Type: Article , PeerReviewed
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  • 67
    Publication Date: 2024-06-27
    Description: Highlights • Alkaline magmas of the TLTF island chain result from a subduction-modified mantle source and two-stage partial melting. • The role of mantle source and parental melt composition for high Cu-Au mineral potentials is important but limited. • A shallow crustal magma reservoir is key for epithermal ore formation. Abstract The Tabar-Lihir-Tanga-Feni (TLTF) island chain in northeastern Papua New Guinea formed by tectonic and alkaline to shoshonitic magmatic activity since the Pliocene. Several volcanic centers are Cusingle bondAu mineralized including the world-class Ladolam Au deposit and Conical Seamount south of Lihir. The latter has been recognized as a juvenile analogue to the Ladolam deposit located on-shore. Whereas the mineralization at Conical Seamount is reasonably well studied, the specific magmatic processes that promote epithermal mineralization at this seamount but not at others are poorly understood. Here, we present new petrological and geochemical data from Conical Seamount, and compare them with those from the barren (unmineralized) Edison, Tubaf and New World seamounts nearby. We focus on whole rock compositions and major and trace element analysis of melt inclusions and minerals including clinopyroxene, sulfide and magnetite. We combine our observations with modelled constraints on mantle source composition and partial melting as well as magma evolution. A first-stage melting leaves a residual mantle source enriched in Au. Second-stage melting of a previously subduction-metasomatized mantle generally promotes the transfer and concentration of metals and volatiles in the ascending melts. These magmas are unlikely to control ore formation as all seamounts show evidence for similar mantle sources and parental melt composition. However, the presence of a shallow crustal magma chamber is unique to Conical Seamount. It is characterized by frequent melt replenishments and extensive magma fractionation leading to sulfide and magmatic volatile saturation. These specific magma chamber processes lead to the pre-enrichment of the magma in chalcophile elements including Au, while sulfide saturation coeval with magmatic volatile exsolution provide the way for an effective Au transfer from the magmatic to the epithermal system.
    Type: Article , PeerReviewed , info:eu-repo/semantics/article
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  • 68
    Publication Date: 2024-06-27
    Description: Non-technical summary Scenarios compatible with the Paris agreement's temperature goal of 1.5 °C involve carbon dioxide removal measures - measures that actively remove CO2 from the atmosphere - on a massive scale. Such large-scale implementations raise significant ethical problems. Van Vuuren et al. (2018), as well as the current IPCC scenarios, show that reduction in energy and or food demand could reduce the need for such activities. There is some reluctance to discuss such societal changes. However, we argue that policy measures enabling societal changes are not necessarily ethically problematic. Therefore, they should be discussed alongside techno-optimistic approaches in any kind of discussions about how to respond to climate change. Technical summary The 1.5 °C goal has given impetus to carbon dioxide removal (CDR) measures, such as bioenergy combined with carbon capture and storage, or afforestation. However, land-based CDR options compete with food production and biodiversity protection. Van Vuuren et al. (2018) looked at alternative pathways including lifestyle changes, low-population projections, or non-CO2 greenhouse gas mitigation, to reach the 1.5 °C temperature objective. Underlined by the recently published IPCC AR6 WGIII report, they show that demand-side management measures are likely to reduce the need for CDR. Yet, policy measures entailed in these scenarios could be associated with ethical problems themselves. In this paper, we therefore investigate ethical implications of four alternative pathways as proposed by Van Vuuren et al. (2018). We find that emission reduction options such as lifestyle changes and reducing population, which are typically perceived as ethically problematic, might be less so on further inspection. In contrast, options associated with less societal transformation and more techno-optimistic approaches turn out to be in need of further scrutiny. The vast majority of emission reduction options considered are not intrinsically ethically problematic; rather everything rests on the precise implementation. Explicitly addressing ethical considerations when developing, advancing, and using integrated assessment scenarios could reignite debates about previously overlooked topics and thereby support necessary societal discourse. Social media summary Policy measures enabling societal changes are not necessarily as ethically problematic as commonly presumed and reduce the need for large-scale CDR
    Type: Article , PeerReviewed
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  • 69
    Publication Date: 2024-06-27
    Description: This study contributes to the inaugural exploration of non-equilibrated Ocean Alkalinity Enhancement (OAE). The manipulation of Total Alkalinity (TA), involving silicate and calcium-based ∆TA gradients ranging from 0 to 600 µmol · L-1, was conducted without prior CO2 sequestration, under natural conditions and at a mesocosm scale (~60 m3). The resulting impact included an increase in pH and a decrease in pCO2, sustained across the experiment, as full natural equilibration via sea-gas exchange did not occur. Implemented in a neritic system under post-bloom conditions, a midway mixing event was simulated. Following an inorganic nutrient addition, discernible delays in bloom formation, as indicated by the Gross Production (GP) and Net Community Production (NCP) rates, as well as by the chlorophyll-a (Chla) concentrations, in relation to the ∆TA gradient, were observed. Notably, the delay was more pronounced for the calcium treatment set compared to the silicate one, where low TA treatments exhibited earlier responses than high TA ones. This delay is likely attributed to the previously documented, species-specific negative relationships between high pH/lowCO2 levels and phytoplankton growth rates. This study underscores the need for further investigation into the implications of this response pattern in terms of trophic transfer and seasonal suitability. Further, it is anticipated that a wider delay in bloom formation would be evident with a larger non equilibrated TA gradient. Thus, highlighting the importance of exploring variations in TA limits for a comprehensive understanding of the OAE’s impacts.
    Type: Article , NonPeerReviewed , info:eu-repo/semantics/article
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  • 70
    Publication Date: 2024-06-27
    Description: Ocean deoxygenation is becoming a major stressor for marine ecosystems. Climate change affects ocean oxygen by altering wind fields and air-sea heat and freshwater fluxes. However, the quantitative contribution of these drivers to ocean deoxygenation remains uncertain. Here, we use a global ocean biogeochemistry model run under historical atmospheric forcing to show that deoxygenation since the late 1960s has been driven mainly by changing air-sea heat and freshwater fluxes and associated changes in solubility and ocean circulation. However, ~60% of this deoxygenation was offset by a wind-driven increase in ventilation and interior oxygen supply, mainly in the Southern Ocean. In the coming decades, the projected slowdown in wind stress intensification, combined with continued ocean warming, could greatly accelerate ocean deoxygenation. While ocean biogeochemistry models under historical atmospheric forcing struggle to reproduce the observed deoxygenation after 2000, fully coupled Earth system models capture the trend, indicating systematic problems in hindcast simulations.
    Type: Article , NonPeerReviewed
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  • 71
    Publication Date: 2024-06-27
    Description: Transparent exopolymer particles (TEP) and Coomassie stainable particles (CSP), two prominent classes of gel−like particles in the ocean primarily produced by phytoplankton, play crucial roles in ecological and biogeochemical processes, influencing microbial nutrition, growth, and particle aggregation. The distribution of these particles is intricately linked to the spatiotemporal dynamics of phytoplankton. Mesoscale cyclonic eddies (CEs) are known to stimulate phytoplankton growth and influence particle transport, but their effects on TEP and CSP remain to be determined. In the Eastern Tropical North Atlantic (ETNA), we examined three CEs: one off the Mauritanian coast during summer (Mau), one offshore during winter (Sal), and another near Brava island during winter. Mau and Brava CEs were in their intensification/maturity phase, while the Sal CE was in its decay phase. Both TEP and CSP concentrations correlated with primary productivity, but TEP increased with chlorophyll−a concentration, whereas elevated CSP coincided also with the highest abundance of pico−nanophytoplankton (〈20 µm), mainly Synechococcus. Both gels exhibited a positive correlation with bacterial biomass production, indicating their consumption by heterotrophic bacteria. TEP total area in the epipelagic waters of all CEs (Mau, Brava, and Sal) was elevated compared to surrounding waters, with on average 4, 2.5, and 1.6−fold higher values, respectively. However, no significant difference in TEP size distribution was observed within any CEs and their surroundings. Similarly, CSP total area increased in the epipelagic waters of Mau and Brava CEs, with on average 5 and 2.4−fold higher values, respectively, compared to surrounding waters. CSP particles were notably larger in these two eddies, while the Sal CE showed no significant difference from surrounding waters in CSP abundance and size. Overall, TEP and CSP exhibited distinct responses to CEs, with increased concentrations during their intensification/maturation stage and remineralization dominating during their decaying stage.
    Type: Article , PeerReviewed , info:eu-repo/semantics/article
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  • 72
    Publication Date: 2024-06-26
    Description: On 4 March 2021, a devastating M8.1 earthquake struck the Kermadec Islands of New Zealand. Given the tremendous energy released during the event, we sought to investigate the event’s potential impact on the ionosphere and the inner Van Allen Belt using data from the high-energy electron detectors on board the NOAA-18 satellite. The survey was also extended to the strongest shallow M6.5+ earthquakes occurring between 150° and 190° in longitude, and between −5° and −35° in latitude over the previous ten years. In nearly all cases, evident electron fluxes entering the loss cone were observed. To explore the possibility of a connection between ionospheric signals and tectonic events in this intensely active region, we analyzed electron losses from the inner Van Allen Belt, taking into account latitude, longitude, day/night times, and proximity to the South Atlantic Anomaly. Compared to previous studies, here only the most significant loss phenomena persistent in the ionosphere were considered. Particular interest was reserved for the intense electron loss events that had a duration spanning from a few to several minutes and occurred several hours before and after strong seismic events. Thereafter, time series of electron counting rates and strong Southern Pacific earthquakes were transformed into binary series, and the series multiplication was investigated. The results suggest four peaks of association, including a first couple between electron perturbations detected for ascending semi-orbits and seismic events and a second one between electron perturbations detected in the southern ionosphere and seismic events. They both anticipated the occurrence of earthquakes, occurring around 4 h before them. Other couples were observed between electron perturbations detected for descending semi-orbits and seismic events and between electron perturbations detected in the northern ionosphere and seismic events. They both occurred around 3 h after the occurrence of earthquakes. The case of perturbations anticipating seismic events has the intriguing properties of sustaining the hypothesis that a physical interaction occurred around 6 h before seismic events as in the West Pacific case. A physical model of electrons detected far several thousands of km from the earthquake epicenters was also presented. However, a simulation of random seismic events suggested that the null hypothesis cannot be fully rejected for these associations, prompting many more analyses and case studies.
    Description: Published
    Description: 1059
    Description: OST2 Deformazione e Hazard sismico e da maremoto
    Description: JCR Journal
    Keywords: South Pacific ; electron bursts ; statistical correlation ; NOAA satellites ; strong earthquakes ; high energy electron bursts
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 73
    Publication Date: 2024-06-26
    Description: Variations in the CO2 dissolved in water springs have long been observed near the epicenters of moderate and strong earthquakes. In a recent work focused on data collected during the 2017–2021 period from a monitoring site in the Northern Apennines, Italy, we noticed a significant correlation between CO2 anomalies and moderate-to-weak seismic activity. Here, we extended this analysis by focusing on data collected from the same site during a different period (2010–2013) and by integrating the CENSUS method with an artificial neural network (ANN) in the already-tested protocol. As in our previous work, a fit of the computed residual CO2 distributions allowed us to evidence statistically relevant CO2 anomalies. Thus, we extended a test of the linear dependence of these anomalies to seismic events over a longer period by means of binary correlations. This new analysis also included strong seismic events. Depending on the method applied, we observed different time lags. Specifically, using the CENSUS methodology, we detected a CO2 anomaly one day ahead of the earthquake and another anomaly eleven days ahead. However, no anomaly was observed with the ANN methodology. We also investigated possible correlations between CO2 concentrations and rain events and between rain events and earthquakes, highlighting the occurrence of a CO2 anomaly one day after a rain event of at least 10 mm and no linear dependence of seismic and rain events. Similar to our previous work, we achieved a probability gain of around 4, which is the probably of earthquake increases after CO2 anomaly observations.
    Description: Published
    Description: 739
    Description: OST3 Vicino alla faglia
    Description: JCR Journal
    Keywords: CO2 anomalies ; continuous monitoring ; small earthquakes ; statistical correlations ; 04.06. Seismology
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 74
    Publication Date: 2024-06-26
    Description: All datasets provided in the operational dataset (Heubeck et al., 2024) of the ICDP project BASE (ICDP 5069) consist of metadata, data and/or images. Here, a summary of explanations of the tables, data and images exported from the database of the project (mDIS BASE) are given and are complimented by additional information on data from measurements done in the laboratory prior to the sampling party. Finally, the sampling data from the first two sam-pling parties are added. Some basic definitions of identifiers used in ICDP, depths corrections and measurements are also introduced.
    Language: English
    Type: info:eu-repo/semantics/report
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  • 75
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    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2024-06-26
    Description: Solar radiation over and under sea ice was measured by radiation station 2014R4, an autonomous platform, installed on drifting Multi-Year-Ice (MYI) in the Arctic Ocean during Oden_AO18. The resulting time series describes radiation measurements as a function of place and time between 20 August 2018 and 20 December 2018 in sample intervals of 3 hours. The radiation measurements have been performed with spectral radiometers. All data are given in full spectral resolution interpolated to 1.0 nm, and integrated over the entire wavelength range (broadband, total: 320 to 950 nm). Two sensors, solar irradiance and upward reflected solar irradiance, were mounted on a on a platform about 1 m above the sea ice surface. The third sensor was mounted 0.5 m underneath the sea ice measuring the downward transmitted irradiance. Along with the radiation measurements, this autonomous platform consisted of thermistor chain with 208 sensors and several other sensor packages, which measured water temperature, pressure and conductivity at hourly intervals. An underwater lightchain measured counts of red, green and blue light at 49 positions at hourly intervals. All times are given in UTC.
    Keywords: 2018R4; Arctic Ocean; Arctic Ocean 2018, MOCCHA; autonomous platform; AWI_SeaIce; buoy; Conductivity; Current sea ice maps for Arctic and Antarctic; drift; drift ice; Ice mass balance; light chain; meereisportal.de; MIDO; Multidisciplinary Ice-based Distributed Observatory; Oden; Oden_AO2018; Oden_AO2018_2018R4; RAD_S; Radiation Station; Sea Ice Physics @ AWI; solar radiation
    Type: Dataset
    Format: application/zip, 69 datasets
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  • 76
    Publication Date: 2024-06-26
    Description: Data presented here were collected during the cruise SO290 with RV SONNE from Nuoméa (New Caledonia) to Nuoméa (New Caledonia) (April 15, 2022 - Mai, 12, 2022). In total, 19 underwater light profiles were collected at 7 stations, using a free-falling hyperspectral light profiler. The system used was a SEABIRD HyperPro II (SN 099, former Satlantic), equipped with a irradiance sensor to measure downward irradiance in water (Ed, SN 262) and a radiance sensor for the upward radiance in water (Lu, SN 227). A reference unit was attached to the ship to measure the downward irradiance in air (Es, SN 223). The sensors were pre-calibrated by the manufacturer and validated prior to the cruise with a reference lamp. Data were recorded with the SatView software (V 2.9.5_7) and processed from raw to Level1, 1b, 2, 2s to Level 3a using the ProSoft Processing software (V 7.7.19_2). Measured data were binned in 0.5 m depth intervals. A dark correction was made automatically based on shutter measurements by the instrument. Measurements with a tilt higher than 5 were not taken into account during processing. Spectra were interpolated to 1 nm intervals. For each station the hyperspectral profiles for each parameter cover the wavelength range from 400-700 nm, for Ed and Es in [W/m nm], for Lu in [W/m nm sr]. For Ed, Lu and Es descriptive statistics are given including min, max, mean, median and standard deviation of the tilt and the photosynthetically active radiation PAR [µmol photons/m² s (sr)], integrated from 400 - 700 nm. To allow an assignment of above water conditions to the respective depth measurements, Es spectra were given as a function of depth, recalculated from data Level2s. The Profiler measurements were only conducted during daylight. Raw data are available on request from the principal investigator.
    Keywords: Ed; Es; hyperspectral; irradiance; Light/Optics; LIOP; Lu; PaläoTaNZ; radiance; SO290; SO290_12-4; SO290_14-4; SO290_1-6; SO290_16-4; SO290_19-5; SO290_3-5; SO290_8-5; Sonne_2; Tasman Sea; underwater light field
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 77
    Publication Date: 2024-06-26
    Description: This data set reports two highly resolved δ¹¹B-derived CO₂ records during the late Pleistocene (0-400 ky) from ODP Sites 999 (Caribbean) and 871 (West Pacific) based on the δ¹¹B of the planktonic foraminifera species Globigerinoides ruber measured by MC-ICPMS (multicollector inductively coupled plasma mass spectrometer). The δ¹¹B-derived CO₂ is tested against the ice core CO₂ record as well as compared with different CO₂ calculation approaches and proxies of local foraminifera dissolution to evaluate drivers of CO₂ offset between the two records. We report (1) δ¹¹B, Mg/Ca and input data for boron-derived CO₂ calculation, (2) Mg/Ca-derived sea surface temperature calculated with various approaches, (3) the effect of Mg/Ca treatment on boron-derived CO₂, (4) δ¹⁸O and δ¹³C of benthic foraminifera and G. ruber, and (5) fragmentation index and sand fraction.
    Keywords: Boron isotope; CO2; Foraminifera; Ocean Drilling Program; ODP; Pleistocene
    Type: Dataset
    Format: application/zip, 6 datasets
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  • 78
    facet.materialart.
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    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2024-06-26
    Description: Solar radiation over and under sea ice was measured by radiation station 2018R1, an autonomous platform, installed on drifting First-Year-Ice (FYI) in the Weddell Sea during PS111_ANT. The resulting time series describes radiation measurements as a function of place and time between 26 February 2018 and 16 November 2018 in sample intervals of 1 hour. The radiation measurements have been performed with spectral radiometers. All data are given in full spectral resolution interpolated to 1.0 nm, and integrated over the entire wavelength range (broadband, total: 320 to 950 nm). Two sensors, solar irradiance and upward reflected solar irradiance, were mounted on a on a platform about 1 m above the sea ice surface. The third sensor was mounted 0.5 m underneath the sea ice measuring the downward transmitted irradiance. All times are given in UTC.
    Keywords: 2018R1; ANT-XXXIII/2; AWI_SeaIce; Current sea ice maps for Arctic and Antarctic; FRAM; FRontiers in Arctic marine Monitoring; meereisportal.de; Polarstern; PS111; PS111_2018R1; RAD_S; Radiation Station; Sea Ice Physics @ AWI
    Type: Dataset
    Format: application/zip, 6 datasets
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  • 79
    Publication Date: 2024-06-26
    Description: To comprehensively document the δ13C content of the South Atlantic Central Water (SACW), we used high-resolution thermocline-dwelling foraminiferal δ13C data obtained from three distinct marine sediment cores situated in the NW, SW, and SE regions of the South Atlantic. Our dataset enables a comprehensive examination of millennial-scale variations in SACW δ13C content across the entire basin. Notably, the thermocline δ13C records from the SE and NW sectors of the South Atlantic consistently exhibit concurrent negative excursions during most of the Heinrich Stadials (HS), a pattern that contrasts sharply with the absence of such negative excursions in the thermocline δ13C record from the SW sector of the South Atlantic
    Keywords: AWI_INSPIRES; Globorotalia inflata; Globorotalia truncatulinoides; iAtlantic; Integrated Assessment of Atlantic Marine Ecosystems in Space and Time; International Science Program for Integrative Research in Earth Systems; Mg/Ca-based sea surface temperature; SACW; South Atlantic; Thermodynamic isotopic air-sea equilibration
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 80
    Publication Date: 2024-06-26
    Description: The helicopter borne probe HELiPOD was deployed during the MOSAiC expedition on Leg 3 and 4 from the research vessel Polarstern to investigate the ocean-ice-atmosphere exchange. During five flights, a variety of parameters were measured and calculated, concerning atmospheric dynamics (pressure, temperature, humidity, wind vector), aerosol particles (number concentrations in different size classes, absorption coefficients for three different wavelengths), trace gas concentrations (carbon dioxide, methane, ozone), radiation (solar and terrestrial, upward and downward), surface properties (temperature, images) as well as flight state parameters (position, altitude, attitude). All data were re-sampled at 100 Hz to the same time grid, if not indicated differently. The probe enabled the spatial extension of MOSAiC observations in a range of 25 – 60 km distance to Polarstern. After dedicated postprocessing of the complex data set, two out of the five flights, which were performed on 22 July 2020, and with a flight duration of around 1 h per flight, are initially uploaded to the PANGAEA data base. A technical overview of the HELiPOD is given in Pätzold et al. (2023).
    Keywords: absorption; aerosol particle number concentration; Arctic; Arctic Ocean; atmospheric boundary layer; helicopter borne probe; Helicopter towed system; HELiPOD; HELIPOD; meteorological parameters; MOSAiC; MOSAiC20192020; MOSAiC expedition; Multidisciplinary drifting Observatory for the Study of Arctic Climate; Polarstern; PS122/4; PS122/4_48-104; PS122/4_48-105; surface properties; trace gas concentrations
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 81
    Publication Date: 2024-06-26
    Description: Solar radiation over and under sea ice was measured by radiation station 2020R12, an autonomous platform, installed on drifting Second-Year-Ice (SYI) in the Arctic Ocean during MOSAiC (Leg 3) 2019/20. The resulting time series describes radiation measurements as a function of place and time between 24 April 2020 and 07 August 2020 in sample intervals of 3 hours. The radiation measurements have been performed with spectral radiometers. All data are given in full spectral resolution interpolated to 1.0 nm, and integrated over the entire wavelength range (broadband, total: 320 to 950 nm). Two sensors, solar irradiance and upward reflected solar irradiance, were mounted on a on a platform about 1 m above the sea ice surface. The third sensor was mounted 0.5 m underneath the sea ice measuring the downward transmitted irradiance. Along with the radiation measurements, this autonomous platform consisted of a lightchain, which measured counts of red, green and blue light at 49 positions at hourly intervals. In addition, the evolution of snow height is measured at hourly intervals. All times are given in UTC.
    Keywords: 2020R12; Arctic Ocean; autonomous platform; AWI_SeaIce; buoy; Current sea ice maps for Arctic and Antarctic; drift; lightchain; meereisportal.de; MOSAiC; MOSAiC20192020; Multidisciplinary drifting Observatory for the Study of Arctic Climate; Polarstern; PS122/3; PS122/3_28-108; PS122/4; PS122/4_43-173; RAD_S; Radiation Station; Sea Ice Physics @ AWI; snow depth; solar radiation
    Type: Dataset
    Format: application/zip, 8 datasets
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  • 82
    Publication Date: 2024-06-26
    Description: Solar radiation over and under sea ice was measured by radiation station 2020R11, an autonomous platform, installed on drifting Second-Year-Ice (SYI) in the Arctic Ocean during MOSAiC (Leg 2) 2019/20. The resulting time series describes radiation measurements as a function of place and time between 26 March 2020 and 01 August 2020 in sample intervals of 3 hours. The radiation measurements have been performed with spectral radiometers. All data are given in full spectral resolution interpolated to 1.0 nm, and integrated over the entire wavelength range (broadband, total: 320 to 950 nm). Two sensors, solar irradiance and upward reflected solar irradiance, were mounted on a on a platform about 1 m above the sea ice surface. The third sensor was mounted 0.5 m underneath the sea ice measuring the downward transmitted irradiance. Along with the radiation measurements, this autonomous platform consisted of a lightchain, which measured counts of red, green and blue light at 49 positions at hourly intervals. In addition, the evolution of snow height is measured at hourly intervals. All times are given in UTC.
    Keywords: 2020R11; Arctic Ocean; autonomous platform; AWI_SeaIce; buoy; Current sea ice maps for Arctic and Antarctic; drift; lightchain; meereisportal.de; MOSAiC; MOSAiC20192020; Multidisciplinary drifting Observatory for the Study of Arctic Climate; Polarstern; PS122/3; PS122/3_28-55; PS122/4; PS122/4_43-158; RAD_S; Radiation Station; Sea Ice Physics @ AWI; snow depth; solar radiation
    Type: Dataset
    Format: application/zip, 7 datasets
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  • 83
    Publication Date: 2024-06-26
    Description: Time series data of physical oceanography (seawater conductivity, temperature, pressure, salinity) and ocean current velocities were obtained from mooring M6 on the upper part (500 m isobath) of the continental slope, just east of the Filchner Trough in the southern Weddell Sea in February 2017 - February 2021. The mooring was deployed during the WAPITI expedition on James Clark Ross (JR16004), and recovered during the COSMUS expedition with Polarstern (PS124). The attached archive contains data from 1 RCM7 (24 meters above bottom (mab herafter) and sampling interval (sint hereafter) 2h), 5 SBE56 (25, 59, 74, 126, 202 mab, sint: 120 s), 3 SBE37 (34, 99, 176 mab, sint: 600 s), 1 RDI ADCP 150 kHz (235 mab, upwardlooking, sint: 1h), 1 SBE39 (15 mab, sint: 900s). Mooring diagrams and information about data processing are provided
    Keywords: ADCP; Antarctica; AWI_PhyOce; Continental Slope; Filchner Region; Filchner Trough; GPF 19-2_039, COSMUS; James Clark Ross; JR16004; JR16004_160; JR16004_160, PS124_99-1; M6_MOOR_WeddellSea; M6, M6_MOOR_WeddellSea; MOOR; Mooring; oceanographic moorings; oceanographic time series; Physical Oceanography @ AWI; Polarstern; PS124; PS124_99-1; Temperature and Salinity; WAPITI; Weddell Sea
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 84
    Publication Date: 2024-06-26
    Description: This data collection of the ~17 m long piston core MR16-09 PC03 contains age pointers for an age model, major element data (Ti, Rb) from an XRF scan, biomarkers (n-alkanes, alkenones and brGDGTs), and d18O from foraminifera (G. bulloides and G. truncatulinoides). The piston core MR16-09 PC03 is located near the southern Chilean continental margin, at a distance of ~150 km. In addition, there are alkenone data (C37:4) from sites GeoB3327 and PS75/034 (Ho et al., 2012), which are located north and south of MR16-09 PC03, respectively, and further away from the Chilean margin.
    Keywords: Alkenone; Biomarkers; brGDGT; Chile; Helmholtz-Verbund Regionale Klimaänderungen = Helmholtz Climate Initiative (Regional Climate Change); MR16-09 PC03; n-alkane; Patagonia; Patagonian Ice Sheet; REKLIM; Sediment core; SST; UK'37; UK37
    Type: Dataset
    Format: application/zip, 9 datasets
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  • 85
    Publication Date: 2024-06-26
    Description: In July 2022 within the framework of an Alfred-Wegener-Institute-managed expedition and the Nunataryuk project, sediment cores were taken at three locations, off the coast of Herschel Island, Canada, using a hand corer: YC22_MR_6: 69°34'23.12N, 138°54'37.76W; 3 m water depth; July 6th 2022 YC22_MR_7: 69°34'23.53N, 138°56'37.66W, 6 m water depth; July 7th 2022 YC22_MR_8: 69°30'22.75''N, 138°53'21.69''W; 45 m water depth; July 24th 2022 Data sets were obtained to investigate carbon feedback from the sediments to the water column and atmosphere, using DIC concentrations and isotopic values. The local sediments are supplied primarily by organic carbon previously stored in adjacent permafrost soils (biomarker and bulk data), which erode and redeposit quickly (age model) on the ocean floor. The acquired data includes: 1) Sediment data: Bulk total organic carbon content (Lamping et al., 2021) and its isotopic values for 13C (Brodie et al., 2011; Werner & Brand, 2001) and 14C (Mollenhauer et al., 2021) and Biomarker data: Quantifying alkanes (CPI) , and fatty acids (TAR ratio) as described by Wei et al. (2020), Glycerol dialkyl glycerol tetraethers (GDGTs basis for BIT-Index) after Hopmans et al. (2016), Hopanes (fßß) following instructions by Meyer et al., (2019), and Sterols (Dinosterol) after Dauner et al. (2022). 2) Porewater was extracted from the cores using rhizomes and quantified as described in Oni et al., (2015). Dissolved inorganic carbon isotope signatures were determined as CO2 for 13C (Torres et al., 2005) and 14C (Mollenhauer et al., 2021). 3) Intact polar lipid fatty acids were extracted from the sediments, purified, and 14C analysis was performed as described in Ruben et al. (2023). The 13C isotopy was determined with GC-IRMS (Elvert et al., 2003). The respective precursor lipids of the polar fraction used for isotope analysis were quantified following the method described in Wörmer et al. (2013). Datasets are to be found at doi:10.1594/PANGAEA.966262 and doi:/10.1594/PANGAEA.966264. 4) Sedimentary age model of core YC22_MR_7 assuming constant rate of supply (CRS) model (Appleby, 2001), based on data obtained with a HPGe gamma detector.
    Keywords: NUNATARYUK; NUNATARYUK, Permafrost thaw and the changing Arctic coast, science for socioeconomic adaptation
    Type: Dataset
    Format: application/zip, 7 datasets
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  • 86
    Publication Date: 2024-06-26
    Description: Field data: Lightness data extracted from core images of gravity corer sediments collected during project Kerguelen Plateau Sediment Drifts with RV Sonne Cruise SO272 in February and March 2020. Red, Green, Blue, Hue, Saturation, Lightness data were extracted from a 5 cm long and 0.2 mm wide area in the core center using the IGOR PRO software. The gravity cores were retrieved from the Labuan and Gaggatt Basin spanning Plio-Pleistocene to Eocene sediments. Lightness data were extracted to characterise the color of the sediment and document changes.
    Keywords: Center for Marine Environmental Sciences; Color, Hue; Color, L*, lightness; Color BLUE; Color GREEN; Color RED; DEPTH, sediment/rock; field data; GC; GeoB24011-1; Gravity core; Gravity corer; IGOR Pro software; Kerguelen Plateau Sediment Drifts; Lightness; MARUM; RV Sonne cruise SO272; Saturation; SO272; SO272_19-1; Sonne_2; Southern Indian Ocean
    Type: Dataset
    Format: text/tab-separated-values, 216774 data points
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  • 87
    Publication Date: 2024-06-26
    Description: Field data: Core images of gravity corer sediments collected during project Kerguelen Plateau Sediment Drifts with RV Sonne Cruise SO272 in 2020. Images of core sections were assambled using custom made IGOR Pro Software Code. The gravity cores were retrieved from the Labuan and Gaggatt Basin spanning Plio-Pleistocene to Eocene sediments. Core Images were generated to characterise the color of the sediment and document changes in color as well as sedimentary structures.
    Keywords: Center for Marine Environmental Sciences; field data; GC; GeoB24001-1; Gravity core; Gravity corer; images; Kerguelen Plateau Sediment Drifts; MARUM; RV Sonne cruise SO272; SO272; SO272_6-1; Sonne_2; Southern Indian Ocean
    Type: Dataset
    Format: image/tiff, 26.4 MBytes
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  • 88
    Publication Date: 2024-06-26
    Description: Field data: Core images of gravity corer sediments collected during project Kerguelen Plateau Sediment Drifts with RV Sonne Cruise SO272 in 2020. Images of core sections were assambled using custom made IGOR Pro Software Code. The gravity cores were retrieved from the Labuan and Gaggatt Basin spanning Plio-Pleistocene to Eocene sediments. Core Images were generated to characterise the color of the sediment and document changes in color as well as sedimentary structures.
    Keywords: Center for Marine Environmental Sciences; field data; GC; GeoB24003-1; Gravity core; Gravity corer; images; Kerguelen Plateau Sediment Drifts; MARUM; RV Sonne cruise SO272; SO272; SO272_10-1; Sonne_2; Southern Indian Ocean
    Type: Dataset
    Format: image/tiff, 26.4 MBytes
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  • 89
    Publication Date: 2024-06-26
    Description: Field data: Core images of gravity corer sediments collected during project Kerguelen Plateau Sediment Drifts with RV Sonne Cruise SO272 in 2020. Images of core sections were assambled using custom made IGOR Pro Software Code. The gravity cores were retrieved from the Labuan and Gaggatt Basin spanning Plio-Pleistocene to Eocene sediments. Core Images were generated to characterise the color of the sediment and document changes in color as well as sedimentary structures.
    Keywords: Center for Marine Environmental Sciences; field data; GC; GeoB24004-1; Gravity core; Gravity corer; images; Kerguelen Plateau Sediment Drifts; MARUM; RV Sonne cruise SO272; SO272; SO272_11-1; Sonne_2; Southern Indian Ocean
    Type: Dataset
    Format: image/tiff, 26.4 MBytes
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  • 90
    Publication Date: 2024-06-26
    Description: Field data: Core images of gravity corer sediments collected during project Kerguelen Plateau Sediment Drifts with RV Sonne Cruise SO272 in 2020. Images of core sections were assambled using custom made IGOR Pro Software Code. The gravity cores were retrieved from the Labuan and Gaggatt Basin spanning Plio-Pleistocene to Eocene sediments. Core Images were generated to characterise the color of the sediment and document changes in color as well as sedimentary structures.
    Keywords: Center for Marine Environmental Sciences; field data; GC; GeoB24005-1; Gravity core; Gravity corer; images; Kerguelen Plateau Sediment Drifts; MARUM; RV Sonne cruise SO272; SO272; SO272_12-1; Sonne_2; Southern Indian Ocean
    Type: Dataset
    Format: image/tiff, 26.4 MBytes
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  • 91
    Publication Date: 2024-06-26
    Description: Field data: Core images of gravity corer sediments collected during project Kerguelen Plateau Sediment Drifts with RV Sonne Cruise SO272 in 2020. Images of core sections were assambled using custom made IGOR Pro Software Code. The gravity cores were retrieved from the Labuan and Gaggatt Basin spanning Plio-Pleistocene to Eocene sediments. Core Images were generated to characterise the color of the sediment and document changes in color as well as sedimentary structures.
    Keywords: Center for Marine Environmental Sciences; field data; GC; GeoB24006-1; Gravity core; Gravity corer; images; Kerguelen Plateau Sediment Drifts; MARUM; RV Sonne cruise SO272; SO272; SO272_13-1; Sonne_2; Southern Indian Ocean
    Type: Dataset
    Format: image/tiff, 26.4 MBytes
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  • 92
    Publication Date: 2024-06-26
    Description: Field data: Core images of gravity corer sediments collected during project Kerguelen Plateau Sediment Drifts with RV Sonne Cruise SO272 in 2020. Images of core sections were assambled using custom made IGOR Pro Software Code. The gravity cores were retrieved from the Labuan and Gaggatt Basin spanning Plio-Pleistocene to Eocene sediments. Core Images were generated to characterise the color of the sediment and document changes in color as well as sedimentary structures.
    Keywords: Center for Marine Environmental Sciences; field data; GC; GeoB24007-1; Gravity core; Gravity corer; images; Kerguelen Plateau Sediment Drifts; MARUM; RV Sonne cruise SO272; SO272; SO272_14-1; Sonne_2; Southern Indian Ocean
    Type: Dataset
    Format: image/tiff, 26.4 MBytes
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  • 93
    Publication Date: 2024-06-26
    Description: Field data: Core images of gravity corer sediments collected during project Kerguelen Plateau Sediment Drifts with RV Sonne Cruise SO272 in 2020. Images of core sections were assambled using custom made IGOR Pro Software Code. The gravity cores were retrieved from the Labuan and Gaggatt Basin spanning Plio-Pleistocene to Eocene sediments. Core Images were generated to characterise the color of the sediment and document changes in color as well as sedimentary structures.
    Keywords: Center for Marine Environmental Sciences; field data; GC; GeoB24008-1; Gravity core; Gravity corer; images; Kerguelen Plateau Sediment Drifts; MARUM; RV Sonne cruise SO272; SO272; SO272_15-1; Sonne_2; Southern Indian Ocean
    Type: Dataset
    Format: image/tiff, 26.4 MBytes
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  • 94
    Publication Date: 2024-06-26
    Description: Field data: Core images of gravity corer sediments collected during project Kerguelen Plateau Sediment Drifts with RV Sonne Cruise SO272 in 2020. Images of core sections were assambled using custom made IGOR Pro Software Code. The gravity cores were retrieved from the Labuan and Gaggatt Basin spanning Plio-Pleistocene to Eocene sediments. Core Images were generated to characterise the color of the sediment and document changes in color as well as sedimentary structures.
    Keywords: Center for Marine Environmental Sciences; field data; GC; GeoB24009-1; Gravity core; Gravity corer; images; Kerguelen Plateau Sediment Drifts; MARUM; RV Sonne cruise SO272; SO272; SO272_16-1; Sonne_2; Southern Indian Ocean
    Type: Dataset
    Format: image/tiff, 26.4 MBytes
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  • 95
    Publication Date: 2024-06-26
    Description: Field data: Core images of gravity corer sediments collected during project Kerguelen Plateau Sediment Drifts with RV Sonne Cruise SO272 in 2020. Images of core sections were assambled using custom made IGOR Pro Software Code. The gravity cores were retrieved from the Labuan and Gaggatt Basin spanning Plio-Pleistocene to Eocene sediments. Core Images were generated to characterise the color of the sediment and document changes in color as well as sedimentary structures.
    Keywords: Center for Marine Environmental Sciences; field data; GC; GeoB24010-1; Gravity core; Gravity corer; images; Kerguelen Plateau Sediment Drifts; MARUM; RV Sonne cruise SO272; SO272; SO272_17-1; Sonne_2; Southern Indian Ocean
    Type: Dataset
    Format: image/tiff, 26.4 MBytes
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  • 96
    Publication Date: 2024-06-26
    Description: Field data: Core images of gravity corer sediments collected during project Kerguelen Plateau Sediment Drifts with RV Sonne Cruise SO272 in 2020. Images of core sections were assambled using custom made IGOR Pro Software Code. The gravity cores were retrieved from the Labuan and Gaggatt Basin spanning Plio-Pleistocene to Eocene sediments. Core Images were generated to characterise the color of the sediment and document changes in color as well as sedimentary structures.
    Keywords: Center for Marine Environmental Sciences; field data; GC; GeoB24011-1; Gravity core; Gravity corer; images; Kerguelen Plateau Sediment Drifts; MARUM; RV Sonne cruise SO272; SO272; SO272_19-1; Sonne_2; Southern Indian Ocean
    Type: Dataset
    Format: image/tiff, 26.4 MBytes
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  • 97
    Publication Date: 2024-06-26
    Description: Multi sensor core logging (MSCL) data from gravity cores retrieved during RV SONNE Cruise SO272 generated at MARUM University Bremen; cores 24001-1, 24003-1, 24006-1, 24009-1, 24011-1. Data: CoreThickness, PwaveAmplitude, PWaveVelocity in m per second, GammaRayAttenuation Density in g per CC, Magnetic Susceptibility in SI10^-5. The gravity cores were retrieved from the Labuan and Gaggatt Basin spanning Plio-Pleistocene to Eocene sediments. MSCL data were generated at 1 cm steps at MARUM using a GEOTEK Multi-Sensor Core Logger, a automated system for measuring bulk density (GRA density), P-wave velocity and magnetic susceptibility at whole and split cores of sediment, in September and Oktober 2021. MSCL Data were obtained to characterise the physical properties of the sediment.
    Keywords: Center for Marine Environmental Sciences; data; Density, wet bulk; DEPTH, sediment/rock; GC; GeoB24001-1; Gravity corer; Kerguelen Plateau Sediment Drifts; Magnetic susceptibility, volume; MARUM; Multi-Sensor Core Logger (MSCL), GEOTEK; Multi sensor core logging data; RV Sonne cruise SO272; Section; Section position; SO272; SO272_6-1; Sonne_2; Southern Indian Ocean; Thickness; Velocity, compressional, amplitude; Velocity, compressional wave
    Type: Dataset
    Format: text/tab-separated-values, 6682 data points
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  • 98
    Publication Date: 2024-06-26
    Description: Multi sensor core logging (MSCL) data from gravity cores retrieved during RV SONNE Cruise SO272 generated at MARUM University Bremen; cores 24001-1, 24003-1, 24006-1, 24009-1, 24011-1. Data: CoreThickness, PwaveAmplitude, PWaveVelocity in m per second, GammaRayAttenuation Density in g per CC, Magnetic Susceptibility in SI10^-5. The gravity cores were retrieved from the Labuan and Gaggatt Basin spanning Plio-Pleistocene to Eocene sediments. MSCL data were generated at 1 cm steps at MARUM using a GEOTEK Multi-Sensor Core Logger, a automated system for measuring bulk density (GRA density), P-wave velocity and magnetic susceptibility at whole and split cores of sediment, in September and Oktober 2021. MSCL Data were obtained to characterise the physical properties of the sediment.
    Keywords: Center for Marine Environmental Sciences; data; Density, wet bulk; DEPTH, sediment/rock; GC; GeoB24003-1; Gravity corer; Kerguelen Plateau Sediment Drifts; Magnetic susceptibility, volume; MARUM; Multi-Sensor Core Logger (MSCL), GEOTEK; Multi sensor core logging data; RV Sonne cruise SO272; Section; Section position; SO272; SO272_10-1; Sonne_2; Southern Indian Ocean; Thickness; Velocity, compressional, amplitude; Velocity, compressional wave
    Type: Dataset
    Format: text/tab-separated-values, 2196 data points
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  • 99
    Publication Date: 2024-06-26
    Description: Multi sensor core logging (MSCL) data from gravity cores retrieved during RV SONNE Cruise SO272 generated at MARUM University Bremen; cores 24001-1, 24003-1, 24006-1, 24009-1, 24011-1. Data: CoreThickness, PwaveAmplitude, PWaveVelocity in m per second, GammaRayAttenuation Density in g per CC, Magnetic Susceptibility in SI10^-5. The gravity cores were retrieved from the Labuan and Gaggatt Basin spanning Plio-Pleistocene to Eocene sediments. MSCL data were generated at 1 cm steps at MARUM using a GEOTEK Multi-Sensor Core Logger, a automated system for measuring bulk density (GRA density), P-wave velocity and magnetic susceptibility at whole and split cores of sediment, in September and Oktober 2021. MSCL Data were obtained to characterise the physical properties of the sediment.
    Keywords: Center for Marine Environmental Sciences; data; Density, wet bulk; DEPTH, sediment/rock; GC; GeoB24006-1; Gravity corer; Kerguelen Plateau Sediment Drifts; Magnetic susceptibility, volume; MARUM; Multi-Sensor Core Logger (MSCL), GEOTEK; Multi sensor core logging data; RV Sonne cruise SO272; Section; Section position; SO272; SO272_13-1; Sonne_2; Southern Indian Ocean; Thickness; Velocity, compressional, amplitude; Velocity, compressional wave
    Type: Dataset
    Format: text/tab-separated-values, 1102 data points
    Location Call Number Expected Availability
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  • 100
    Publication Date: 2024-06-26
    Description: Multi sensor core logging (MSCL) data from gravity cores retrieved during RV SONNE Cruise SO272 generated at MARUM University Bremen; cores 24001-1, 24003-1, 24006-1, 24009-1, 24011-1. Data: CoreThickness, PwaveAmplitude, PWaveVelocity in m per second, GammaRayAttenuation Density in g per CC, Magnetic Susceptibility in SI10^-5. The gravity cores were retrieved from the Labuan and Gaggatt Basin spanning Plio-Pleistocene to Eocene sediments. MSCL data were generated at 1 cm steps at MARUM using a GEOTEK Multi-Sensor Core Logger, a automated system for measuring bulk density (GRA density), P-wave velocity and magnetic susceptibility at whole and split cores of sediment, in September and Oktober 2021. MSCL Data were obtained to characterise the physical properties of the sediment.
    Keywords: Center for Marine Environmental Sciences; data; Density, wet bulk; DEPTH, sediment/rock; GC; GeoB24009-1; Gravity corer; Kerguelen Plateau Sediment Drifts; Magnetic susceptibility, volume; MARUM; Multi-Sensor Core Logger (MSCL), GEOTEK; Multi sensor core logging data; RV Sonne cruise SO272; Section; Section position; SO272; SO272_16-1; Sonne_2; Southern Indian Ocean; Thickness; Velocity, compressional, amplitude; Velocity, compressional wave
    Type: Dataset
    Format: text/tab-separated-values, 1883 data points
    Location Call Number Expected Availability
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